Authors:
Tătaru D., Toma-Dănilă D., Năstase E.

Abstract:
Over the last few years, science has advanced unprecedentedly in explaining phenomena and facts with a high impact on society: earthquakes for example. On the other hand, new technologies are transforming the way (seismological) information is collected and transmitted to public and other various stakeholders categories. From interactive multimedia content to immersive experiences, difficult concepts become easier to be transmitted and understood by a wide variety of audience, starting with children, a most important part of tomorrow?s society. But what if the aiming is far more than captivating young people or promoting science and scientific results? How can we, scientists, deliver information in such a way that awareness and mitigation comes immediately after or even together with learning and understanding? For a quake-prone country, earthquakes have to be a major and continuous concern, but depending on the recurrence period of damaging events, effective measures for mitigation might not be disregarded but considered as top priority. Romania is a good example, with an average of 2-3 earthquakes with magnitude greater than 7 per century. Although the seismic hazard was recently reevaluated and ranked one in the top of hazards with the greatest impact on population and economy, and also giving that questionnaires indicated that people are most afraid of earthquakes, the preparedness actions are very slow in Romania. One of the reasons lie in the fact that people forgot what an earthquake can do (as they also did prior to the 1940 and 1977 events). That is why special tools are necessary to address the needs for education and awareness in a technologically oriented society. In a world where information delivered through social media travels much faster than seismic waves, scientists need to adapt and be more present as an authoritative and relevant source of information. In this context, a partnership that brings together the unique expertise of geoscientists, visual designers and digital content developers was established, in order to develop and deliver a modern and innovative product: a Mobile Earthquake Exhibition (MOBEE). MOBEE aims to mobilize wide public as well as media and decision makers to increase earthquake preparedness by delivering and wisely spreading earthquake information and scientific explanations related to this natural hazard. The exposition makes use of new digital technologies (mobile apps, mapping tools or touch screen devices) but also explores the interplay between science and art, or more precisely how visual art can help better explain and transmit science concepts and generate new research and visual communication tools about seismic safety.

Authors:
Tătaru D., Poiată N., Grecu B.

Abstract:

Authors:
Moldovan I.A., Toader V.E., Moldovan A.S., Ghica D., Constantin A.P.

Abstract:
he atmospheric sound waves with frequencies lower than 20Hz are named infrasound waves. Among the multitude of infrasonic signals that have been recorded and detected during time, some of them have been associated with different natural or anthropogenic sources and the source of many other remaining hidden and unknown. At the beginning of year 2013, a permanent infrasound monitoring system composed by a MB AZEL2007 microbarometer, the digitizer and the transmitting equipment, was installed by NIEP, at Mangalia, Romania, on the Black Sea coast line (at 50m from the water front) to test the infrasonic method in correlation with local, regional, and global sources producing acoustic waves with frequencies lower than 20Hz. Five years of recordings show at lower frequencies (less than 2Hz) a predictable behavior of infrasonic activity on the seashore, suggesting the presence of highly coherent infrasound waves in atmosphere. At higher frequencies (2Hz-8Hz) there appeared a type of waves that was never recorded before by our infrasonic sensors in other locations far away from the sea shore. The interesting aspect on the spectrogram resides in well defined, visible superior harmonics of the dominant signal, which develops between 2 and 8Hz. These harmonics are clear and create the specific spider legs aspect present in spectrograms. The precise source of these high amplitude signals at higher frequencies is under investigation and a couple of suppositions have been made. One of them refers to the composition of atmosphere that might be possible to act as a band pass filter which selects certain preferred frequencies from the background infrasonic noise induced by water's surface. The propagation parameters of this filter may be altered by aerosols concentration, humidity, temperature and, perhaps, by other factors. The corroboration of the infrasound recordings and spectrograms with local meteorological data show a good correlation between the spectrogram and the daily variation of the humidity parameter.

Authors:
Constantin A.P., Moldovan I.A., Lavigne F., Grancher D., Partheniu R.

Abstract:
Tsunami is one of the major natural hazards presenting significant flood risk for coastal communities and therefore, increasing the society resilience to this phenomena in exposed areas is very important for minimizing damage and possible destructive effects on the environment in these areas. In the frame of the EC Programme-FP7 ASTARTE project (Assessment, STrategy And Risk reduction for Tsunamis in Europe), we conducted a questionnaire survey among people living, working, or visiting Eforie Nord site. The tsunami questionnaire has been translated in Romanian language, the questions referring to: interviewee's relation to Eforie Nord site, information about interviewed people, tsunami hazard knowledge/risk perception, evacuation issue, awareness of the existing warning system, information, and communication. The results obtained after the survey confirm that coastal communities from Romania are not resilient to tsunami hazard. Our respondents have mentioned from natural and anthropic types of hazards, the tsunami as third rank in Eforie Nord test site, coming after earthquakes and storms. Whatever the respondent?s status (i.e. local population, or tourists), earthquakes and sea withdrawal are cited as tsunami warning signs by 62% and 60% of the respondents, respectively. Regarding the perception of a future tsunami event in Eforie Nord, 36.3% of the respondents think that the place could be affected by a tsunami and the tsunami wave could reach more than 2-5 meters (heights cited by approx. 14% of respondents) or even more than 5-10 meters (values cited by 15% of interviewed people).

Authors:
Năstase E.I., Muntean A., Ionescu C., Mocanu V., Ambrosius B.A.C

Abstract:
A decade of improvements and new development of tools for observation statistics, standard point positioning, clock-jumps and cycle-slip detection and other interruptions over all constellations, frequencies and signals, satellite elevations and azimuths, elevation-specific histograms, satellite ascending/descending times for horizon and user elevation cut-off, pseudo-range multipath and noise, carrier-phase signal-to-noise ratio, data gaps and small data pieces and other useful lists and statistics allow us to analyze in detail the GNSS data collected for one of the main research subjects resulted from the September 2013 unique seismic swarm event that occurred in Romania. Open-source software such as: G-Nut/Anubis (Geodetic Observatory Pecn?), RTKLIB, gLAB (European Space Agency) and commercial software like: Leica Spider QC, Leica Geo Office are used for quality control over all available data of the Ph.D. thesis called ?An integrated GNSS and seismotectonic study of the NW Galati seismogenic area?. The main purpose of the paper is currently the quantity and quality monitoring of all available GNSS data achieved in 4 years of continuous monitoring along with the solutions obtained from the 4 GPS measuring campaigns (2013-2016), i.e. signals, frequencies and satellite constellations.

Authors:
Bălă A.

Abstract:

Authors:
Bălă A., Tătaru D., Grecu B.,

Abstract:
Tectonic of Romania includes both pre-alpine platforms and Alpine orogenic structures. The pre-alpine platforms are: Eastern European Platform, with its western margin in Romania—Moldavian platform; Scythian platform; Moesian platform.

Authors:
Constantinescu E. G., Diaconescu D., Grecu B.

Abstract:
This paper presents a basic description of the geological and tectonic setting of the areas of placement of four seismological observatories located in the eastern part of Romania. The four seismological observatories are MLR ? Red Mountain Seismologic Observatory, NEHR ? Nehoiu Mountain Seismological Observatory, ODBI ? Odobesti Seismological Observatory and VRI ? Vrancioaia Seismological Observatory. This observatories were chose because of their importance and proximity to the seismic active Vrancea region. Many geologic studies, of this areas, were carried out through time, resulting in a vast literature, studies, several geologic sections and maps. This descriptions were compiled from the geologic and tectonic maps, geologic sections, studies and literature, mentioned above, for every location of the observatories. For each one, of the sites, a geotectonic map was drawn, showing the main geologic formations and tectonic features. This geotectonic information was synthetized to add a better view to the lithological and tectonic history of each of the sites. Through this paper, we hope to provide clearer information and understanding of the geology and tectonics in which the mentioned observatories are set.

Authors:
Craiu A., Craiu M., Mihai M., Diaconescu M., Ghiță C.

Abstract:
Catalog of focal mechanisms for Vrancea (Romania) intermediate depth earthquakes (2005-2017)

Authors:
Craiu A., Dăneț A., Mihai M., Craiu M., Mărmureanu A.

Abstract:
One of the main objectives in real-time assessment of seismic hazard is the development of algorithms for rapid estimation of the seismic source parameters (fault planes solutions). The objective of this work is to test and implement new methodologies in the National Institute for Earth Physics (NIEP) for near real time estimation of fault planes solutions taking the advantage of the spatial density of the Seismic Network in seismically active zones ( 120 seismic stations used in real time) and the full range of tools used. To determine fault planes solutions was implemented the FPL code (code that generates parameters: strike, dip, rake, etc.) in ANTELOPE 5.6, software developed by Kinemetrics This code (FPL) uses the classic criteria to determine the focal mechanisms, namely P wave polarities, systematic tests of all possible fault plane solutions, so will validate only those solutions who met the required criteria. Another cod- Psmeca -is a code developed in GMT, which reads data values from files and generates PostScript code that will plot a focal mechanism on a map. These programs were implemented in the routine analysis ANTELOPE 5.6 software. Estimating the near-real-time fault planes solutions using dedicated programs, a few minutes after the event occurrence is done by generating locations of the seismic events with magnitude ML?4 for seismic events occurred at intermediate depths (H?60 km).

Authors:
Besuțiu L., Manea V.C., Pomeran M.

Abstract:
To avoid shortcomings of the current models attempting to explain genesis of the Vrancea intermediate-depth earthquakes the alternative model of an unstable triple junction (VTJ) had been previously proposed mainly based on a speculative approach. The paper deals with results of the latest research, including high-resolution seismic tomography obtained through the joint inversion of seismic and gravity data, and numerical modelling of the mantle convection that brings new evidence to support VTJ as a valid alternative for Vrancea intermediate-depth seismicity geodynamic setting. Of a special interest proved to be the advanced numerical modelling run on a High Performance Computing Cluster own by Solid Earth Dynamics Department in the Institute of Geodynamics of the Romanian Academy that has demonstrated how a stable triple lithospheric contact may transform into an unstable triple junction under the influence of a thermal anomaly even in the absence of differences between the plates velocities.

Authors:
Craiu M., Gallo A., Costa G., Dăneț A., Craiu A.

Abstract:
The seismicity of Romania is significantly affected by earthquakes produced by the Vrancea seismic source with intermediate depth events (3 shocks/century with magnitude Mw greater than 7.0). The seismic activity on the Romanian territory consists of both shallow and intermediate-depth earthquakes. The crustal seismicity is moderate and more scattered in comparison with the intermediate-depth one. The recent upgrade of the seismic network in Romania with high dynamic range accelerometers ( 114 real time seismic stations equipped with episensors) allows recording of moderate to large magnitude earthquakes at very close epicentral distances (less than 10-20 km). Strong motion data of high quality are also of help in increasing the effective preparation against seismic disasters, and the response during seismic emergencies. The consequent increased ability of a community to quickly recover from the damages of an earthquake thus contributes to lower the seismic risk, usually measured in term of casualties and economic losses. During 2016 in this seismic area were recorded two moderate events with 5.7 magnitude in September respectively December. The purpose of this work consists mainly in the estimation of moment magnitude Mw using the strong motion network of the NIEP. A stable and automatic method was developed by Gallo et al.,2014, has been implemented in the real time data acquisition and processing system (ANTELOPE) to estimate in real time the seismic moment, the moment magnitude and the corner frequency of events recorded by accelerometers, using Andrews (1986) method applied to S waves. The main goals are the independent estimation of seismic moment and the common characterization for all events recorded by the strong motion network.

Authors:
Diaconescu M., Craiu M.G., Oros E., Craiu A., Constantinescu E.G.

Abstract:
The paper highlights the seismicity of the Strei-Hateg depressionary system. This system is situated in the western part of the Southern Carpathians, and consists of two intermountain, post orogenic basins, Hateg basin and Strei basin. These two basins are separated by a threshold. The seismicity is characterized by moderate magnitude with a maximum magnitude of 4 (Mw) (8 September 2013) and by the presences of the seismic sequences. In the area are known two seismic sequences, one in 2011 of 14 earthquakes of 2 to 3.3 magnitude, main shock of 3.3 (Mw) and one in 2013 of 30 earthquakes with magnitude of 2 to 4 (Mw), main shock of 4 (Mw). The hypocentral depths are in 5 to 13 km depth interval with two exceptions, one earthquake with 19.6 km hypocentral depth (2013/09/08) and the other with 23.8 km hypocentral depth (2013/09/11). The sequence of March 2011 is a seismic swarm, with three shocks of 3.1, 3.2, 3.3 (Mw) and the other shocks between an interval of 1.9?2.4 (Mw). The sequence of September 2013 has an earthquake of magnitude 4.0(Mw) considered as a main shock. It was preceded by 9 foreshocks and followed by 25 aftershocks. The focal mechanisms of the earthquakes indicate a strike slip predominant movement with slight normal or inverse components.

Authors:
Ghiță C., Craiu A., Craiu M.G., Diaconescu M., Mărmureanu A.

Abstract:
The moderate-size earthquake with local magnitude 5,7 which occurred on November 22, 2014 in Vrancea region, at 41 km depth, is the largest crustal event instrumentally recorded at the bending of the Eastern Carpathians. Using the method developed by [2] termed the Hash method, (incorporated in Seisan software) we obtain the focal mechanisms for earthquakes that occurred in Vrancea region associated with the seismic sequence of November 22, 2014. We have examined the main shock and 29 aftershocks that occurred after 22 November 2014. P-wave arrivals and polarities are manually identified on the vertical component of each station. Polarities are marked as impulsive or emergent and the pick is given a quality rating (0- 4). We then use the S/P amplitude ratios computed from three?component seismograms, to determine mechanisms- Hash [2]. We had also investigate the spatial variation in focal mechanism type (e.g. strike-slip, normal, or thrust) and inferred fault strike. Most of the mechanisms are normal faulting, with the nodal planes oriented SE - NW, in agreement with the tectonic characteristics of the zone.This crustal seismicity is related to the normal fault system associated to Peceneaga - Camena major fault, which separates the Focsani Basin, part of the Moesian Platform, from the North Dobrogea promontory.

Authors:
Grecu B., Neagoe C., Partheniu R., Năstase E., Zaharia B.

Abstract:
In this paper, we analyze almost ten years of continuous recordings (November 2007? April 2017) from 114 stations of the Romanian Seismic Network using the power spectral densities and their corresponding probability density functions (PSD PDF). For each vertical station component, we compute the statistical mode for noise levels from the PSD PDFs. The noise mode represents the highest probability noise level for a given station. We then construct the PSD PDF mode low-noise model for Romania (RONM) from the minimum of all the noise modes at each period. The RONM is shown to be very close to the Peterson?s (1993) new low noise model. The diurnal and seasonal variations of the RONM are also shown. Finally, we compare our mode noise model with those obtained in similar way in different parts of the world: Greece, New Zealand and United States. We consider the RONM as a more realistic reference model for future installations of seismic stations in Romania and for assessing the performance of the existing ones.

Authors:
Grecu B., Toma-Dănilă D., Tătaru D., Ionescu C., Dăneț A.

Abstract:
Earthquakes represent a real threat in Romania. They can cause important damages, loss of lives, socio-economic as well as cultural losses. The National Institute for Earth Physics (NIEP) is the only governmental organization responsible for monitoring the seismic activity on Romania?s territory. NIEP provides different kind of information minutes to hours after the occurrence of a significant earthquake in Romania: near realtime information (location, depth and magnitude), ground shaking parameters and maps with the intensity of the shaking, post-event parameters, reports and macroseismic intensities. To issue such information, NIEP has been developing since 1980 one of the largest seismic networks in Europe, the Romanian Seismic Network (RSN). At present, RSN consists of 115 seismic stations equipped with velocity and accelerometer sensors and two seismic arrays. The increase of the density of the stations within RSN in the last decade led to a significant increase of the number of seismic events detected and located in Romania. RSN also provides valuable information for emergency managers in case of earthquake disaster, as it can provide rapid initial estimates and updated estimates of the location and extend of damage.

Authors:
Muntean A., Ambrosius B.A.C, Mocanu V., Năstase E.I., Ionescu C.

Abstract:
In this paper we present the results of an analysis of 15 years of continuous GNSS/GPS measurements in Romania. The purpose of this work is threefold: monitoring of crustal changes occurring in the Romanian territory in correlation with tectonic processes in South-East Europe (Africa-Europe plate interaction), observation of crustal movements in order to establish the surface-to-depth relationship of deep earthquakes in the area of the Eastern Carpathians bend zone (Vrancea region) and improving the accuracy of the coordinates of the national seismic network stations. The development of the Romanian GNSS/GPS (Global Navigation Satellite System/Global Positioning System) network started in 2001 when the first permanent station was installed at Lacauti in the Vrancea seismogenic area. Since then the network has grown to 27 stations covering the entire Romanian territory and is still expanding. In our analysis we also include 18 GNSS stations of the GeoPontica network, developed and maintained by the National Research and Development Institute for Marine Geology and Geoecology, with the purpose to monitor geodynamic processes in the Western Black Sea coastal area. It consists of 13 stations in Romania and 5 in Bulgaria. In this paper we provide a comprehensive description of the GPS networks, reflecting the actual capabilities, justifying implementation choices and presenting the results. The GPS data were processed in daily batches with the ?precise point positioning? (PPP) strategy using the GIPSY-OASIS software. From the resulting position timeseries the horizontal and vertical motion vectors were calculated relative to a stable Eurasian reference frame. The results of our study show that internally the Romanian territory appears to be quite stable, but the whole country trends to move slightly southward relative to Eurasia at velocity rates of about 2.5 ? 3.0 mm/yr, especially the southern part. We speculate that this is a far-field effect of slab roll-back due to the subduction of the African plate under the Eurasian plate at the Aegean trench, way to the south. Until now, we did not observe any long-term signals due to the deep Vrancea earthquakes because the effects on surface motion are probably small, but we will do more detailed studies of some recent (2016) Mw 5.3 seismic events in the Vrancea area.

Authors:
Neagoe C., Grecu B., Radulian M.

Abstract:
The focal mechanism and rupture directivity for intermediate-depth earthquakes occurred in the Vrancea source (Romania) are determined using FMNEAR algorithm [1]. The method is based on the waveform inversion of near-source seismic waveforms and on a linear finite source model. When the FMNEAR algorithm is started the first parameters that are determined are the moment magnitude (Mw), the double couple focal mechanism (strike, dip, rake) and the distribution of seismic moment along strike. This provides a first order estimate of rupture length and directivity. The depth of the source is also explored. A band-pass filter is automatically applied for each individual component of the recorded waveform (N, E, Z). The inversion is made in successive steps combining grid searches for (strike, dip, rake) parameters and simulation to determine rupture onset times and the shape of the local source time functions. Also a confidence index is defined. The method was tested on seismic events with magnitude higher than Mw = 3.5 recorded by the Romanian seismic network (broadband stations and accelerometers). Tests were made on events recorded by a large number of welldistributed stations and also for less favorable cases to evaluate the capability of the algorithm to constrain focal mechanism and source time function. In its present configuration, FMNEAR method is implemented in near real-time.

Authors:
Neagoe C., Grecu B., Manea L. M.

Abstract:
National Institute for Earth Physics (NIEP) has started the development of its own realtime seismic network since 2002. The network is designed to monitor the seismic activity on Romania territory, which is dominated by intermediate earthquake from the Vrancea area. In present the network consist of 115 seismic stations and two seismic array. The seismic stations are equipped with Quanterra Q330 or Basalt digitizers, broad-band seismometers (STS2, CMG40T, CMG 3ESP, CMG3T, PBB-200s) or shortperiod sensors (MARK L4C, MARK L22, RANGER). Most of the velocity sensors are collocated with Episensors Kinemetrics acceleration sensors. The processing software used by the National Data Center are Antelope and Seiscomp3. The program used for the automatic real-time locations in this study is Seiscomp3. Seedlink which is a part of Seiscomp3 is used for data acquisition in real time and also for data exchange. The automated software was tuned to obtain the most accurate location for the earthquakes and avoiding any false events. Different parameters were tested (like: STA/LTA, filters applied to the waveforms) on a data set of earthquakes representative for the local seismicity. Now Seiscomp3 is running in real time and detected over 300 seismic events. NIEP has developed a web application that uses the data stored in the database to display earthquake information, like location, magnitude and depth in real time. Another use for the data collected is to create and maintain contact lists to which datacenter sends notifications (email), based on the parameter of the earthquake. NIEP plans is to develop the means to cross-check the data generated between the different analysis systems. (e.g. comparing data generated by Antelope with data generated by Seiscomp).

Authors:
Oros E., Constantinescu E.G., Diaconescu M., Popa M.

Abstract:
The active stress pattern in the Apuseni Mts area is investigated and studied in relation to the local seismicity and geology. Our analysis is based on several high quality and resolution data bases obtained recently in the context of national and international projects and which refers to digital seismograms recorded by dense networks, parametric earthquakes catalogues and catalogues of focal mechanisms. The reduced stress tensor has been obtained by formal inversion of 89 focal mechanisms solutions. The maximum horizontal stress SHmax directions and tectonic regime change at local scale displaying a very heterogeneous stress field and claiming a major influence of local sources of stress. SHmax has systematic reorientations from NE-SW on the western border of the region to E-W in the South, NW-SE in the North and roughly N-S at the tectonic contact between orogenic structures with Transylvanian Depression. The stress and tectonic regimes show clear variations from a pure strike-slip in the structures of Pannonian Depression to extensions all over in the Apuseni Mountains, except the South Transylvanian Fault System area where an extensional strike-slip regime has been computed. The study area is characterized by a very low level of seismicity with a few scattered epicenters in the region or distributed in small clusters mainly on the borders where large neotectonic structures develop (grabens, faults). The study was completed with geodetic data and a seismotectonic model that brings new informations for understanding the seismic hazard and geodynamical processes in the study region.

Authors:
Rogozea M., Ghiță C., Radulian M., Glavcheva R., Toma-Dănilă D.

Abstract:
The Vrancea zone is an area of concentrated seismicity at intermediate depths (60-200 km) beneath the bending area of the South-Eastern Carpathians in Romania. The purpose of the paper is first to find historic data related to the four selected Vrancea earthquakes occurred on 26 November 1829 (Mw 7.3), 1 May 1893 (Mw 6.2), 17 August 1893 (Mw 7.1) and 31 August 1894 (Mw 7.1). Next, to gather all available historic information about those events, analyze it, assess/or convert the intensity using the Medvedev-Sponheuer-Karnik (MSK-64) scale. Further, to compile corresponding macroseismic maps for these earthquakes applying an optimized interpolation method (Kriging). The macroseismic effects distribution has been compared to the distribution of intensity in cases of instrumentally registered strong 20th century Vrancea events of 1940 (Mw 7.7), 1977 (Mw 7.4) and 1986 (Mw 7.1) in order to highlight possible correlation between the main earthquake parameters ? magnitude, source depth and macroseismic intensity

Authors:
Apostol B.F.

Abstract:
The notions of ‘elementary’ seismic sources and ‘elementary’ earthquakes are introduced, as being associated with ‘elementary’ tensorial point forces with a -like time dependence (where is the Dirac delta function). The tensorial character of these forces, known in Seismology as the dipole (or double-couple) representation, is given by the tensor of the seismic moment. A regular seismic source and a regular earthquake can be represented as a superposition of elementary sources and, respectively, elementary earthquakes, governed by a space-time structure factor of the seismic focal region. All these are new concepts. Elementary seismic sources are considered here for a homogeneous isotropic elastic half-space bounded by a free plane surface, the sources being located at an inner point in the half-space. A transient regime of generation and propagation of seismic waves is identified, as distinct from the stationary regime of elastic vibrations. This is another new concept. It is shown that elementary seismic sources produce (double-shock) spherical-shell waves (in the wave region), which are the well-known and waves associated with the feeble tremor in the recorded seismograms. Their mathematical expression, derived here from the tensorial force, differs from known, particular cases. These waves are called here collectively ‘primary’ waves. It is shown that the primary waves interact with the surface of the half-space, where they give rise to ‘secondary’ wave sources, placed on the surface. The secondary waves generated by the secondary sources (which may be called ‘surface seismic radiation’) are estimated here in a simplified model. It is shown that the secondary waves have a delay time in comparison with the primary waves and give rise to a main shock and a long seismic tail, in qualitative agreement with the seismic records. The secondary wave introduced here is a new concept; the main shock and its long tail derived here are elements of novelty. Similarly, the secondary waves generated by an internal discontinuity in the elastic properties of the half-space (an interface parallel with the free surface) are also estimated; it is shown that the discontinuity reduces appreciably the singular main shock on the free surface of the homogeneous half-space.

Authors:
Toader V.E., Moldovan I.A., Mărmureanu A., Ionescu C.

Abstract:
This paper describes the modalities of detection of events in a multidisciplinary network that monitor seismicity, telluric field, magnetic field, electric-electrostatic field, radio ULF waves, air ionization, radon concentration, solar radiation, infrasound, light and acoustic phenomena, meteorological parameters, air-earth temperatures, satellite data with application in seismic Vrancea area (bending zone of Carpathians mountains). The most part of data analysis is automatically done into a distributed structure. Methods used are general but the measured parameters have to be adapted to particularities of monitoring area. Vrancea is a complex zone characterized by intermediate depth earthquakes concentrated and distributed on several levels deep. Data acquisition is followed by their analysis (detection, effects evaluation) and automatic transmission of alerts to beneficiaries specialized in emergency situations (Inspectorate for Emergency Situations, organizations involved in managing special events). Network monitoring allows tracking of climate change and it sends information in real time.

Authors:
Toma-Dănilă D., Armaș I., Cioflan C.O.

Abstract:
The assessment of seismic risk for transportation networks is a difficult task, due to its complexity, hard to get detailed data, lack of methods with low uncertainties and difficulty of defining inter-relations. Through this paper we identify viable ways of analysing the seismic risk of transportation networks in Romania, considering the availability and characteristics of specific data, the possibilities of adapting external knowledge and recently developed methodologies. Until now there was no coherent and complex approach in Romania for this task, referring to the bigger picture. Therefore, we propose an integrative framework that incorporates GIS capabilities (like the ones provided by the ArcGIS Network Analyst Toolbox) and test it for Bucharest. This framework can provide answer to important questions, like “which are the critical segments of networks” or “what could the implications of connectivity loss be?” in case of an earthquake. The approach relies on using fragility functions for critical structures like bridges and tunnels, on empirical formulas for estimating damage level, traffic flow characteristics or connectivity analysis. Results are depicted through multiple performance indicators.

Authors:
Zaharia B., Grecu B., Tătaru D., Oros E.

Abstract:
We propose to investigate the local seismic events in the western part of Romania using data from the SCP experiment, a joint project between University of Leeds, UK and National Institute for Earth Physics, Romania (South Carpathian Project – SCP), using 33 broadband seismic stations autonomously that operated in the western part of the country and continuously recorded data for two years (2009-2011). The seismicity in this area is characterized by shallow activity of moderate magnitude (magnitude below 6) earthquakes with frequent multiple sequences. Tectonically, the region is divided into blocks and basins bordered by intra-crustal faults. The major structural features developed in the region are: the Pannonian Basin with a thin subsiding lithosphere (cca 60 km) and four Dacidic units (Inner Dacides (ID), Transilvanides (T), Middle Dacides (MD), Marginal Dacides (MaD) and Outer Dacides (OD)) with a thicker lithosphere (100 - 140 km), uplifted by recent orogeny. These structures outcrop in the mountain chains and extend westward under the sedimentary cover of the Pannonian Depression. The newest (Neotectonic) tectogeneses were extensional (syn-rift phase) and compressional (basin inversion) resulting in brittle structures: grabens and horsts, separated by NW-SE oriented faults, affecting both the basement and the sedimentary cover. Two Neogene NW-SE oriented major grabens developed at the basement level of the Pannonian Basin: Sannicolau Mare in the West and Caransebes in the East. These structures are extended in the mountains as small depressions, controlled by Neogene normal faults, with the basement lowered down to over 7 km (at Hungary - Romania border). We applied the Wadati method to estimate the Vp/Vs ratio and used it to retrieve a P-wave velocity model for the investigated region. For a better constraint of local seismic events locations, we used the derived P-wave velocity model to relocate all the events using Joint Hypocentral Determination (JHD) method.

Authors:
Aldea A., Radulian M.

Abstract:
The seismic activity in Romania is dominated by the earthquakes generated at intermediate depths (60÷180 km) in the Vrancea region, located at the bend of the South-Eastern Carpathians. The seismicity concentrates in a narrow high-velocity lithospheric volume embedded in the upper mantle. The rate of seismic moment per volume, ~ 0.8 x 1019 Nm/yr, is comparable to southern California (Wenzel et al., 1998). The event produced on 10th November 1940 (Mw = 7.7) was the largest instrumentally recorded earthquake in Romania, was felt in several other countries ( Bulgaria, Republic of Moldova, Ukraine, Russia, Greece, Turkey, Hungary, Yugoslavia, etc.) and produced victims and damage on a wide area beyond Romania’s borders. The large magnitude, the huge macroseismic field (with seismic intensities reaching X), the relatively large number of victims, altogether rank the Vrancea 1940 earthquake as one of the major European seismic events.

Authors:
Zaharia B., Șerbu F., Tătaru D., Grecu B., Năstase E.

Abstract:

Authors:
Apostol B.F.

Abstract:
The displacement caused in an isotropic elastic half-space by a point force localized on or beneath its surface is calculated here by a new method. These classical problems are known as Boussinesq and, respectively, Mindlin problems. The motivation for the present work resides in the fact that the original solutions involve some particular procedures, required by the complexity of the boundary conditions, which may limit their general application. The solutions presented here are obtained by including in a generalized Poisson equation the values of the function and its derivatives on the boundary, and by using in-plane Fourier transforms. This method is general and can be extended to other, similar problems.

Authors:
Apostol B.F.

Abstract:
The representation of a localized faulting seismic source is reformulated, without resorting to the mechanical torque interpretation of the seismic moment tensor. A volume seismic source is introduced by means of the pressure exerted in a small spherical cavity. The elastic waves equation with localized (point) sources is discussed in an isotropic half space bounded by a plane surface, including the boundary conditions. The near-field approximation is used to get the solution of a quasistatic deformation, and the transient regime of far-field propagating elastic waves is discussed for the (time-pulse) seismic sources introduced here. The far-field approximation (waves region) is also presented.

Authors:
Ardeleanu L., Neagoe C.

Abstract:
A primary objective of the national seismic network operated by the National Institute for Earth Physics of Bucharest is the monitoring of the seismic activity on the territory of Romania. As a result of a considerable effort carried out during the past years, mainly since 2008, the network consists at present of 118 permanent digital stations – 99 stations with real time data transmission and 19 offline stations – distributed over the whole territory of the country. The goal of this study is to evaluate the contribution of the on-line network stations to the monitoring of the local normal depth seismicity. During the period January 1, 2008 – June 30, 2013, 5933 events with depth < 60 km and local magnitude ML ≥ 1.2 – earthquakes and quarry blasts – have been localized within the Romanian borders, or in their immediate vicinity, using the data of the national network. To estimate the effectivity of the individual stations we take into consideration the fraction of events localized using the station records (compared to the total number of events of the catalogue, which occurred during the time of station operation), and the location of the station site with respect to the shallow depth seismic sources. The analysis provides a measure of the overall network performance regarding the monitoring of the local seismic activity, and allows us to quantify the value of the individual stations for the localization of the seismic events on the territory of Romania; this information is crucial for decisions regarding the effectiveness increasing and future development of the national network.

Authors:
Ardeleanu L., Neagoe C.

Abstract:
The seismic survey of the territory of Romania is mainly performed by the national seismic network operated by the National Institute for Earth Physics of Bucharest. After successive developments and upgrades, the network consists at present of 121 permanent stations equipped with high quality digital instruments – 102 real time and 19 off-line stations – which cover the whole territory of the country. The goal of this study is to evaluate the individual contribution of the real time seismic stations to the monitoring of the intermediate depth seismicity of the Vrancea region, the seismogenic zone which controls the seismic hazard at regional scale. During the period January 1, 2008 – June 1, 2013, 1468 subcrustal earthquakes (depth ≥ 60 km) with local magnitude ML ≥ 1.3 were localized at the bend of the Eastern Carpathians, using the records of the national network. The performance of each station is estimated by taking into consideration the fraction of events that are localized using the station records, compared to the total number of events of the catalogue, which occurred during the time of station operation. The location of the site and the recovery rate of reliable data are essential elements in the evaluation of the individual station effectiveness.

Authors:
Armaș I., Ionescu R., Gavris A., Toma-Dănilă D.

Abstract:
Measuring seismic vulnerability is a complex and valuable endeavor. It allows us to focus resources where they are critically needed. In this research a variety of data was used to identify the most vulnerable areas in Bucharest in case of an earthquake. Socio-economic data from censuses in 2002 and 2011 were used to generate an overall spatial vulnerability index, while other variables such as earthquake scenarios and distance to resilience-enhancing points in space (e.g., parks, fire stations, etc.) helped to fine-tune the analysis and offered a comprehensive picture of where vulnerability hotspots can be found in an urban environment. The top three most vulnerable hotspots are analyzed and two underlying reasons for their vulnerability are proposed and discussed in more detail: education and connectedness. We applied uncertainty and sensitivity analyses to assess the stability of the results for the vulnerability hotspots. The general outcome of the research is an increase in the overall socio-economic vulnerability in the city in spite of the upward economic trend in the period of time under analysis. Some key challenges about the origins of vulnerability are raised.

Authors:
Bălă A., Tătaru D., Grecu B., Răileanu V.

Abstract:
Moesian Platform is an old massif in the SE Europe bordered to the north and west by the South Carpathians, to the south by the Balkans, to the east by the Black Sea and to the NE by the North Dobrogean Orogen and Scythian Platform. In the Romanian sector, placed north of the Danube river topography of platform shows elevations of 100 - 200 m. Basement of the platform is divided by the Intramoesian Fault in two tectonic sectors, which are different both in age and in composition: the Wallachian sector to the west and the Dobrogean sector to the east. The Dobrogean sector of the patform is prolonged to the east until the Black Sea in the Central and Southern Dobrogea units. Two fault systems cross the platform: one major system is parallel to the Carpathians and accommodates the sinking of platform under Carpathian Orogen; the other fault system is relatively transverse to the first, separating a succession of fault blocks. Sedimentary cover has a variable thickness from a few hundred meters to 10 km or more in Focsani basin. The top of basement was mapped in the last decade using seismic and well data. The crust is thinner in the south and thicker in the north of the platform down to 40-45 km. Crustal investigation of the platform was accomplished in several stages, using in general active seismic investigations. Several large angle seismic crustal lines were recorded and interpreted in the 1970’ years in the E and W part of the Moesian Platform. After 1990 some near-vertical reflection seismic profiles were recorded in the process of oil and gas exploration. Two large angle regional refraction lines (Vrancea’99 and Vrancea2001), having 240 km and 400 km respectively in length, crossed a large part of the platform. New studies on crustal structure are based on the receiver functions method and surface wave inversion applied to the earthquake data. Data are provided by the broad band seismic stations. A preliminary interpretation of the Ps phases indicates depths of 35 km for Vrincioaia station, 33 km for Targusor (TIRR). Comparing the RF and refraction results is observed a slight underestimation of Moho in VRI (-3 km) using receiver function method. The new crustal data lead to review the old crustal models allow the geophysicist researchers to propose a new improved one. The new model comprises a more detailed topography of the surfaces of Moho and top of lower crust across of platform. The new crustal model provides as well a distribution of the mean P-wave velocities within the upper and lower crystalline crust in the whole platform. The new model displays mean P-wave velocities of 5.9-6.4 km/s in upper crystalline crust and 6.6-7.0 km/s in lower crust. The depth of Moho is variable from 30 km in S to 45 km in NE

Authors:
Bălă A., Tătaru D., Grecu B., Toma-Dănilă D.

Abstract:
As a result of the continuous development in the last ten years of the network of the permanent broadband stations in Romania, valuable data for seismicity and crustal structure studies is now available, especially for the western part. Complementary to this national dataset, maintained and developed in the National Institute for Earth Physics, new data emerged from temporary networks established during the joint projects with European partners in the last decades. Such a joint project between University of Leeds, UK and National Institute for Earth Physics, Romania (South Carpathian Project - SCP), deployed 33 broadband seismic stations autonomously operated in an area covering the western part of the country and which continuously provided data for two years (2009-2011). This project offered a good opportunity to study the crustal structure of western part of Romania. The receiver function technique and a joint inversion method of receiver function and Rayleigh wave dispersion are employed in order to derive the 2D seismic velocity models for several seismic station locations. The results show a thin crust for stations located in the eastern part of Pannonian Basin (28-30 km). The stations within the Southern Carpathians are characterized by crustal depths of about 31-36 km. In the Apuseni Mountains the Moho discontinuity is replace by a transition zone extended between 31 to 33 km depth. Models of the variation of the seismic velocity in depth are developed along 3 lines crossing the western part of Romania. On the first 2 lines the Moho limit is placed and it coincide generally with the isoline of seismic transverse velocity of about 3.75 km/s.

Authors:
Bălă A., Toma-Dănilă D.

Abstract:
Bucharest is among the European capitals most vulnerable to earthquakes. Although located at a relatively large epicentral distance (about 140–160 km) from Vrancea area, Bucharest has suffered much destruction and loss of life during great Vrancea earthquakes. In the last century, November 10th, 1940 earthquake (Mw = 7.7) caused the completely collapse of Carlton building located in the central city area, killing over 300 people, and many other high buildings were affected in capital city as in other cities closer to the epicenter. More than 1000 people were killed in a matter of minutes in all Romania during the earthquake, while city of Panciu was destroyed in 90–95 % proportion. This was the moment when the first alarm signal regarding the introducing of mandatory regulations in the seismic design of buildings came out. However, the recommendations made by the specialists were largely ignored by the authorities of the time, so that the next major earthquake of March 4, 1977 (Mw = 7.4) caused the biggest recorded disaster in the history of Bucharest The earthquake of 1977 caused only in Bucharest the collapse of 32 buildings, 8–12 floors high, while about 150 old buildings, with 4–6 floors were badly damaged. Most of the collapsed buildings were built between the 1920 and 1940, they did not benefit of the anti-seismic design. In the case of Bucharest the buildings have been previously damaged in the 1940 earthquake and during the bombardments in the World War II. Over 1500 people died and about 7500 were wounded, most of them in Bucharest City. The total cost of the damage amounted to more than 2 billion dollars, two thirds being related to the capital city only. The aim of the paper is to present aspects related to the consequences of the Vrancea 1940 and 1977 earthquakes, highlighting the differences between the two catastrophic events and their consequences. Therefore everything learned from the past should not be forgotten in order to insure that the next catastrophic event will find a better prepared society.

Authors:
Bălan S.F., Poncos V., Teleagă D., Toma S.A., Apostol B.F.

Abstract:

Authors:
Behr Y., Clinton J., Cauzzi C., Hauksson E., Jonsdottir K., Craiu M.G., Pinar A., Salichon J., Sokos E.

Abstract:
The feasibility of earthquake early warning (EEW) is now widely recognized. However, EEW systems that are in operation or under evaluation worldwide have significant variations and are usually operated independently of routine earthquake monitoring. We introduce a software that allows testing and evaluation of a well‐known EEW algorithm directly within a widely used earthquake monitoring software platform. In the long term, we envision this approach can lead to (1) an easier transition from prototype to production type EEW implementations, (2) a natural and seamless evolution from very fast EEW source parameter estimates with typically large uncertainties to more delayed but more precise estimates using more traditional analysis methods, and (3) the capability of seismic networks to evaluate the readiness of their network for EEW, and to implement EEW, without having to invest in and maintain separate, independent software systems. Using the Virtual Seismologist (VS), a popular EEW algorithm that has been tested in real time in California since 2008, we demonstrate how our approach can be realized within the widely used monitoring platform SeisComP3. Because this software suite is already in production at many seismic networks worldwide, we have been able to test the new VS implementation across a wide variety of tectonic settings and network infrastructures. Using mainly real‐time performance, we analyze over 3200 events with magnitudes between 2.0 and 6.8 and show that, for shallow crustal seismicity, 68% of the first VS magnitude estimates are within ±0.5 magnitude units of the final reported magnitude. We further demonstrate the very significant effect of data communication strategies on final alert times. Using a Monte Carlo simulation approach, we then model the best possible alert times for optimally configured EEW systems and show that, for events within the dense parts of each of the seven test networks, effective warnings could be issued for magnitudes as small as M 5.0.

Authors:
Alexandrescu M., Bălan F.S.

Abstract:
The paper aims to present the first scientific events organized by the Romanian Academy that marked the academic interests in our country to explain the Principle of d’Alembert. The protagonists of this approach (D. Pompei (years 1914–1943) and Șt. Hepites in 1914) were related to the presentation of d’ Alembert`s basic ideas expressed in his „Traité de Dynamique” published in 1743 in which the author does not explicitly for mulate the famous principle that would bear his name and did not use the notion of „force of inertia”. In these circumstances the explanation of the Principles of d’Alembert bearing a strong didactical character has not engaged a debate of ideas, as only target was the primary form of d’Alembert’s contribution to the reformulation of the fundamental law of classical mechanics that Newton had formulated a century before. Through its Mathematics Section, Academy of Sciences organ ized a symposium on December 15th 1945 in the Mechanics Laboratory of the University of Bucharest. Two communications were presented „Forces of inertia in the light of the principles of dynamics” and „The phenomenon of inertia”, first by D.Germani, and the second by C. Budeanu. V.Vâlcovici, at the end, as the ini tiator, organizer and host of the event was pleased to declare an identity of views of the two outstanding relevant previous speakers, expressed in different ways, and richly illustrated through examples from various technical fields, interpreted competently and with power of persuasion. The paper presents in detail all these scientific approaches in theoretical mechanics, in the early twentieth century.

Authors:
Borleanu F., Grecu B., Popa M., Radulian M.

Abstract:
During the last decade Romanian Seismic Network has been significantly improved. A total number of 114 3-C seismic stations and the 2 seismic arrays ensure a good coverage of seismically active regions. As a consequence, the detection threshold decreased allowing location with higher accuracy of low magnitude (ML ~1.0) seismic events. This led to a contamination of Romanian earthquakes catalog with artificial events occurred in different regions. The goal of the present study is to apply various discrimination methods like: spectral and amplitude ratio techniques, complexity factor evaluation and a multi-parameter discriminant on a data set characterized by lower magnitudes events recorded between 2011 and 2015. The selected data consists of small events occurred in the northern part of Romania in the neighborhood of Bucovina array (BURAR). The analysis was carried out on the waveforms recorded with a high signal to noise ratio using the vertical short period array components. Our results revealed that despite of some overlapping, these techniques show a good capacity to discriminate artificial by natural events for the study region.

Authors:
Cioflan C.O., Iancovici M.

Abstract:
This chapter includes papers that deal with the seismic evaluation and rehabilitation of existing buildings in Romania and neighboring countries- e.g. Republic of Moldova, using both fundamental and cutting-edge approaches.

Authors:
Cioflan C.O., Toma-Dănilă D., Manea E.F.

Abstract:
One of the strongest earthquake in Romania was the Vrancea earthquake on 10 November 1940, with moment magnitude 7.7 and depth of 150 km. This event caused significant losses over a wide territory, up to Iasi and Craiova cities. The number of casualties in Romania was around 593 dead and 1271 injured and 65,000 homes were destroyed. A major questions nowadays is: “What could the consequences of a similar earthquake be?”. Through this paper we try to provide insights, by relying on the newly implemented System for Estimating the Seismic Damage in Romania (SeisDaRo), operated by National Institute for Earth Physics (NIEP). This system uses the Improved-Displacement Capacity Analytical Method implemented in the SELENA Software for expressing building loss probabilities. The building database (at city or commune level) is classified into 48 types (depending on construction material, height and age), each with a specific capacity and fragility curve. For this paper we also compute casualty estimates. In the absence of real seismic recordings from the 1940 earthquake we obtained hazard parameters through different ground motion prediction equations (developed by Sokolov, Marmureanu or Vacareanu) specific for the Vrancea intermediate-depth source. Also we test the possibility of using data converted from intensity to acceleration. The damage estimates are represented on relevant maps. Our results show that an earthquake like the one on 1940 could lead to significant damage in our times.

Authors:
Clinton J., Zollo A., Mărmureanu A., Zulfikar C., Parolai S.

Abstract:
European researchers and seismic networks are active in developing new approaches to earthquake early warning (EEW), implementing and operating test EEW systems, and in some cases, offering operational EEW to end users. We present the key recent developments in EEW research in Europe, describe the networks and regions where EEW is currently in testing or development, and highlight the two systems in Turkey and Romania that currently provide operational systems to a limited set of end users.

Authors:
Constantin A.P., Moldovan I.A., Craiu A., Radulian M., Ionescu C.

Abstract:
On November 22, 2014 at 21:14:17 local hour (19:14:17 GMT) a ML=5.7 crustal earthquake occurred in the area of Marasesti city of Vrancea county (Romania) - the epicenter was located at north latitude 45.87° and east longitude 27.16°, with a focal depth of 39 km. This earthquake is the main shock of a sequence that started with this and lasted until the end of January. During the sequence, characterized by the absence of foreshocks, a number of 75 earthquakes were recorded in 72 hours, the largest of which occurred in the same day with the main shock, at 22:30 (ML= 3.1). The crustal seismicity of Vrancea seismogenic region is characterized by moderate earthquakes with magnitudes that have not exceeded MW 5.9, this value being assigned to an earthquake that occurred in historical times on March 1, 1894 (Romplus catalogue). Immediately after the 2014 earthquake occurrence, the National Institute for Earth Physics (NIEP) sent macroseismic questionnaires in all affected areas, in order to define the macroseismic field of ground shaking. According to macroseismic questionnaires survey, the intensity of epicentral area reached VI MSK, and the seismic event was felt in all the extra-Carpathian area. This earthquake caused general panic and minor to moderate damage to the buildings in the epicentral area and the northeast part of country. The main purpose of this paper is to present the macroseismic map of the earthquake based on the MSK-64 intensity scale.

Authors:
Constantin A.P., Partheniu R., Moldovan I.A.

Abstract:
Between years 2001 and 2004 a number of earthquakes with magnitudes which ranged from 3.9 to 5.0 occurred in the most seismically active areas of the Romanian territory. A macroseismic analysis of the effects produced on the Romanian territory has been conducted for these earthquakes, by using macroseismic questionnaires. Some of the observed intensities were significantly higher than those we could have expected after the earthquakes with such magnitudes. Effects have been evaluated from macroseismic observations giving maximum intensities estimated as VI–VII and VII in the MSK scale, respectively. Given the small to moderate size of earthquakes, many of the observed damages to buildings are due to their bad state, age, and poorly built without antiseismic protection, and hence particularly vulnerable.

Authors:
Craiu A., Diaconescu M., Craiu M.G., Mărmureanu A., Ardeleanu L.

Abstract:

Authors:
Craiu A., Diaconescu M., Craiu M.G., Mărmureanu A., Ionescu C.

Abstract:
The goal of this study is to analyze the seismic activity of the Vrancea intermediate depth source zone during the period 2010–2015, time interval when the data provided by the National Seismic Network reached high quantitative and qualitative levels. The Vrancea undercrustal source (60–200 km depth) is located in a small focal volume at the Carpathian Bend, and it dominates the seismicity of Romania. The data set consists of 1603 earthquakes with local magnitudes 1.8 ≤ ML ≤ 5.5, recorded between January 2010 and October 2015. The events were localized using ANTELOPE software for data acquisition and processing. The reliable P-wave polarities were used to estimate the focal mechanism of 80 earthquakes with ML ≥ 3.8.

Authors:
Craiu M.G., Craiu A., Mărmureanu A.

Abstract:
The seismic activity on the Romanian territory consists of both crustal and intermediate-depth earthquakes. The crustal seismicity is moderate and more scattered compared to the intermediate-depth one. In this paper we study the problem of homogeneous determination of local magnitude for earthquakes from the main seismic zones of Romania (Vrancea, Fagaras Mountains, Banat, Transylvania, Dobrogea and Romanian Plain). A waveforms database of digitally recorded data is used to derive new magnitude relations for different seismic areas of Romania. WoodAnderson amplitudes are computed from the available data and the maximum peak-to-peak amplitudes are measured on the horizontal components of the broad-band sensors to define the local magnitude scale. The duration magnitude (MD) is used as reference to calibrate the new magnitude scale based on amplitudes. The new coefficients are estimated through a multiple regression method. Our tests show that the new magnitude scale significantly improves the earthquake size evaluation and stability compared to the solution computed by present-day procedures at the National Institute for Earth Physics.

Authors:
Craiu M.G., Gallo A., Costa G., Mărmureanu A., Craiu A.

Abstract:

Authors:
Apostol A., Moldoveanu T., Sarlea A., Toader V.E.

Abstract:

Authors:
Diaconescu M., Craiu A., Toma-Dănilă D., Craiu M.G.

Abstract:
The study area is located at the contact between the Apuseni Mountains (Western Carpathians) with Pannonian Depression-to the west and with Transylvanian Depression - to the east. The eastern limit is marked by the Eastern Carpathians. The current tectonic activity is manifested by an uplift of the Carpathian Orogeny in relation to neighboring units, particularly the Pannonian Depression. The main seismological active areas are on the edge of the Pannonian Basin and in contact with the basement of Apuseni Mountains and Eastern Carpathians. Historical data suggests two potential earthquake magnitudes Mw >6, one of magnitude 6.2 (Mw) and one with magnitude 6 (Mw). Generally, the characteristics earthquakes of the area have magnitude Mw≤5.6. We expect that the horizontal components of the movement (generated by the uplift of the Carpathians) to produce a compressive stress, as shown by focal mechanism solutions.

Authors:
Diaconescu M., Craiu M.G., Craiu A.

Abstract:
In the present paper, we highlighted the two active seismogenetic zones, one of them to the north–east of Campulung city, and the other one along Ialomita River (west from Sinaia). Schematically we can say that the Southern Carpathians, between the Dambovita and Olt Valleys, are represented by the Supragetic Nappe, which has been over thrust on the Getic nappe during Middle Cretaceous. The Moesian Platform represents a Precambrian block involved in the Epihercynian European Platforms and is composed by three different segments, bounded by the Intramoesian and Calimanesti-Tg. Jiu crustal faults, the Dobrudjean, the Valachian and Danubian domains respectively. The Eastern Carpathians represent the central part of the Outer Carpathians belt and stretch from North to the junction with the Southern Carpathians along Intramoesian Fault. In the studied areal we covered all these units mentioned above and the main faults which mark the areal are Intramoesian Fault(IF) and Calimanesti-Tirgu Jiu fault, also there are a number of the medium to high angle reverse faults, thrust faults and strike slip to transpressional fault zones having a NW-SE direction. More of the earthquakes are located around six major seismogentic areas, such as: Campulung city, Sinaia city, Ialomita River, Targului Valley, Arges Valley and a W to E seismological line in Fagaras mountains.

Authors:
Ghica D.V., Grecu B., Popa M., Radulian M.

Abstract:
In order to discriminate between quarry blasts and earthquakes observed in the Dobrogea seismogenic region, a seismo-acoustic analysis was performed on 520 events listed in the updated Romanian seismic catalogue from January 2011 to December 2012. During this time interval, 104 seismo-acoustic events observed from a distance between 110 and 230 km and backazimuth interval of 110–160° from the IPLOR infrasound array were identified as explosions by associating with infrasonic signals. WinPMCC software for interactive analysis was applied to detect and characterize infrasonic signals in terms of backazimuth, speed and frequency content. The measured and expected values of both backazimuths and arrival times for the study events were compared in order to identify the sources of infrasound. Two predominant directions for seismo-acoustic sources’ aligning were observed, corresponding to the northern and central parts of Dobrogea, and these directions are further considered as references in the process of discriminating explosions from earthquakes. A predominance of high-frequency detections (above 1 Hz) is also observed in the infrasound data. The strong influence of seasonally dependent stratospheric winds on the IPLOR detection capability limits the efficiency of the discrimination procedure, as proposed by this study.

Authors:
Grecu B., Borleanu F., Tătaru D., Zaharia B., Neagoe C.

Abstract:
The characteristics of the background seismic noise recorded at a temporary seismic network have been analyzed using power spectral density estimates and their corresponding probability density functions (PDFs). The network was installed in Bucharest area for 10 months, between November 2003 and August 2004, and consisted of 32 seismic stations equipped with broadband velocity sensors. We investigated the noise level variations as a function of time of day and season. At high frequencies (> 1 Hz), seismic noise shows important diurnal variations for most of the stations, while in the microseismic domain (0.05 – 0.5 Hz) the noise level increases during the colder months of the year. A new approach to compute the horizontal to vertical (H/V) ratios and identify the resonant frequencies was introduced too. The H/V ratios determined from the median of the PDF show similar results, in terms of resonant frequencies, with those obtained when using noise data to compute the spectral ratios. Two resonant peaks, one with larger amplitude and one with smaller amplitude, were identified in the frequency bands 0.13 – 0.3 Hz and 0.5 – 0.9 Hz, respectively.

Authors:
Luzi L., Puglia R., Russo E., D'Amico M., Felicetta C., Pacor F., Lanzano G., Ceken U., Clinton J., Costa G., Duni L., Farzanegan E., Gueguen P., Ionescu C., Kalogeras I., Ozener H., Pesaresi D., Sleeman R., Strollo A., Zare M.

Abstract:
This article describes the Engineering Strong‐Motion Database (ESM), developed in the framework of the European project Network of European Research Infrastructures for Earthquake Risk Assessment and Mitigation (NERA, see Data and Resources). ESM is specifically designed to provide end users only with quality‐checked, uniformly processed strong‐motion data and relevant parameters and has done so since 1969 in the Euro‐Mediterranean region. The database was designed for a large variety of stakeholders (expert seismologists, earthquake engineers, students, and professionals) with a user‐friendly and straightforward web interface. Users can access earthquake and station information and download waveforms of events with magnitude≥4.0 (unprocessed and processed acceleration, velocity, and displacement, and acceleration and displacement response spectra at 5% damping). Specific tools are also available to users to process strong‐motion data and select ground‐motion suites for code‐based seismic structural analyses.

Authors:
Manea E.F., Michel C., Poggi V., Fah D., Radulian M., Bălan F.S.

Abstract:
Large earthquakes from the intermediate-depth Vrancea seismic zone are known to produce in Bucharest ground motion characterized by predominant long periods. This phenomenon has been interpreted as the combined effect of both seismic source properties and site response of the large sedimentary basin. The thickness of the unconsolidated Quaternary deposits beneath the city is more than 200 m, the total depth of sediments is more than 1000 m. Complex basin geometry and the low seismic wave velocities of the sediments are primarily responsible for the large amplification and long duration experienced during earthquakes. For a better understanding of the geological structure under Bucharest, a number of investigations using non-invasive methods have been carried out. With the goal to analyse and extract the polarization and dispersion characteristics of the surface waves, ambient vibrations and low-magnitude earthquakes have been investigated using single station and array techniques. Love and Rayleigh dispersion curves (including higher modes), Rayleigh waves ellipticity and SH-wave fundamental frequency of resonance (f0SH) have been inverted simultaneously to estimate the shear wave velocity structure under Bucharest down to a depth of about 8 km. Information from existing borehole logs was used as prior to reduce the non-uniqueness of the inversion and to constrain the shallow part of the velocity model (<300 m). In this study, we use data from a 35-km diameter array (the URS experiment) installed by the National Institute for Earth Physics and by the Karlsruhe Institute of Technology during 10 months in the period 2003–2004. The array consisted of 32 three-component seismological stations, deployed in the urban area of Bucharest and adjacent zones. The large size of the array and the broad-band nature of the available sensors gave us the possibility to characterize the surface wave dispersion at very low frequencies (0.05–1 Hz) using frequency–wavenumber techniques. This is essential to explore and resolve the deeper portions of the basin. The horizontal to vertical spectral ratio (H/V) curves provide important additional information about the structure and are here characterized by two major peaks. The first is attributed to the fundamental frequency of the basin, while the second can be interpreted as a mixture of the second higher mode of Rayleigh waves and other types of waves such as SH waves. This hypothesis has been verified by comparing the H/V curves with the SH-wave transfer function from the retrieved velocity structure. We could also approximate the SH transfer function with H/V ratios of earthquake recordings, providing additional verification of the robustness of the proposed velocity model. The Cretaceous bedrock depth was then inverted at each URS station from the fundamental frequency of resonance and using this model. A 3-D geophysical model for Bucharest has been constructed based on the integration of the inverted velocity profiles and the available geological information using a geographic information system.

Authors:
Mărmureanu G., Cioflan C.O., Mărmureanu A., Manea E.F.

Abstract:
Vrancea earthquake on November 10th, 1940 (MW = 7.7; MGR = 7.5; h = 150 km; E = 1.122 × 1023 ergs, Imax = IX½) represents the first large earthquake in the last century and was preceded by other earthquakes as: October 22, 1940 (MW = 6.5) and November 8, 1940 (MW = 5.9). If recorded, it would be given the opportunity to get basic data for seismic hazard assessment and useful conclusions for seismic design of structures to strong earthquakes. Unfortunately, no seismic ground motion was recorded and, as a consequence, no improvements of the Romanian design building code were made after this earthquake. The earthquake of November 10, 1940 confirms the existence of deep earthquakes in Vrancea area, deeper than Moho discontinuity in the lower lithosphere, and this theory was developed for the first time by H. Jeffreys in 1935. Focşani city and several municipalities (Coteşti, Panciu etc.) were almost destroyed and the houses not taller than one floor, were completely damaged. More than 45 churches and monasteries were damages, destroyed or demolished. New data regarding damages at monasteries have been synthesized and analyzed, the resulting intensities are completing the known macroseismic field and data may be used to construct the isoseismic map of the maximum possible Vrancea earthquake.

Authors:
Mărmureanu G., Mărmureanu A., Manea E.F., Toma-Dănilă D., Vlad M.

Abstract:
Seismic hazard is quantified by three parameters: level of severity, and spatial and temporal measurements. Thus, the purpose of a seismic hazard assessment is to determine these three parameters from instrumental, historical and geological observations. The characterization of earthquake ground motion for engineering applications generally involves the use of empirical models referred to as groundmotion prediction equations (GMPEs). In classic seismic hazard analysis, this GMPE describes a relationship between a ground motion parameter Y (PGA, PGV, MMI) in site, earthquake magnitude M, source-site distance R, and uncertainty or residual δ. Nothing on epicenter ground acceleration (PGA), velocity (PGV), MMI intensity. Selection of a ground motion for engineering design and other considerations requires a clear understanding of seismic hazard among stakeholders, seismologists and engineers in particular. The authors are coming with data in connection to strong and deep Vrancea earthquakes, the large uncertainties of peak ground accelerations (PGA) recorded in epicenter and far of epicenter in extra-Carpathian area after last three strong earthquakes (August 30,1986; MW = 7.1; h = 131.4 km; May 30,1990; MW = = 6.9; h = 90.9 km; May 31,1990; MW = 6.4; h = 86.9 km). There are many PGA records in Romanian and Republic of Moldavia seismic stations. Many of them are larger than in epicenter Vrâncioaia seismic station. Consequently, classic seismic hazard analysis is not applicable at all to strong and deep Vrancea earthquakes.

Authors:
Moldovan I.A., Diaconescu M., Popescu E., Radulian M., Toma-Dănilă D., Constantin A.P., Plăcintă A.O.

Abstract:
In this study we have used the most reliable and homogeneous seismic datasets at the European scale, covering historical and modern instrumental seismicity until present days for the Eastern part of Romania and the Black Sea Area for computing the statistical parameters of seimogenic sources and assessing the probabilistic hazard in the South Eastern part of Romania

Authors:
Armaș I., Toma-Dănilă D., Ionescu R., Gavriș A.

Abstract:
In this research, we calculate the probability and scale of population losses that may occur due to earthquake hazard in Bucharest. Losses are quantified in direct relation to the social vulnerability of people who are exposed to an earthquake event. Social vulnerability is based on index construction, using spatial decision rules to assess weights in a criteria tree using the SMCE-module of Ilwis software. To estimate building vulnerability, we used the Improved Displacement Coefficient analytical method in the SELENA software. For the earthquake loss estimation, we used the percentage of severely damageable residential buildings in each census unit (CU). The population loss estimation for the selected earthquake scenarios was obtained by multiplying the complex social vulnerability index with the estimated ratio of severely damageable buildings, for three selected earthquake scenarios and using the population numbers in each census unit. The maps represent the maximum affected population values, per census unit, in percentages. We provide useful estimates of the scale and severity of injuries, and link these with current levels of medical preparedness. In all scenarios, the CUs forming the Rahova neighbourhood revealed high loss values, due to significant problems in terms of the built environment and social vulnerability.

Authors:
Muntean A., Mocanu V., Ambrosius B.A.C.

Abstract:
The Petrosani basin is a large and important coal mining zone in the South Carpathians area of Romania. In recent times, most mines have been closed, but an extensive and dense network of galleries still exists. Most of the abandoned ones were not filled in with mine tailings. There is strong concern and evidence that the old galleries are collapsing and/or filling up with water, leading to significant surface deformation and potential hazards, especially for the local communities. We present an analysis of GPS data from nineteen (19) campaign sites spanning the period 2007–2012. Our results are quite consistent and show significant horizontal and vertical surface motions. The horizontal velocities range from 0 to 260 mm/year (mainly in WSW direction), while the vertical velocities range from +39 (uplift) to −263 (subsidence) mm/year. The largest motions appear to be associated with the central (oldest) sector of the mining area. The pattern of vertical motions suggests that the peripheral area is affected by slight uplift in response to the subsidence of the central sector.

Authors:
Năstase E., Muntean A., Ionescu C., Mocanu V., Ambrosius B.A.C.

Abstract:

Authors:
Năstase E., Muntean A., Toma-Dănilă D., Mocanu V., Ionescu C.

Abstract:

Authors:
Năstase E., Oikonomou C., Toma-Dănilă D., Haralambous H., Muntean A., Moldovan I.A.

Abstract:
We examine the lithosphere-atmosphere-ionosphere interaction with respect to earthquake events using Total Electron Content (TEC) data deriving from the Romanian permanent GPS network by applying three different techniques: a) estimation of TEC deviations from the mean state, b) Cross-Correlation Analysis and c) Spectral Analysis. The analysis concerns four seismic events that took place in Romania with magnitude ranging from 5.2 to 6.0. The aim is to identify and study possible ionospheric precursory phenomena linked to these seismic events.

Authors:
Neagoe C., Grecu B., Manea L.M.

Abstract:

Authors:
Daniel Paulescu, Maria Rogozea, Mihaela Popa, Mircea Radulian

Abstract:
The aim of this paper is to describe a managing system for a unique Romanian database of historical seismograms and complementary documentation (metadata) and its dissemination and analysis procedure. For this study, 5188 historical seismograms recorded between 1903 and 1957 by the Romanian seismological observatories (Bucharest-Filaret, Focşani, Bacău, Vrincioaia, Câmpulung-Muscel, Iaşi) were used. In order to reconsider the historical instrumental data, the analog seismograms are converted to digital images and digital waveforms (digitization/ vectorialisation). First, we applied a careful scanning procedure of the seismograms and related material (seismic bulletins, station books, etc.). In a next step, the high resolution scanned seismograms will be processed to obtain the digital/numeric waveforms. We used a Colortrac Smartlf Cx40 scanner which provides images in TIFF or JPG format. For digitization the algorithm Teseo2 developed by the National Institute of Geophysics and Volcanology in Rome (Italy), within the framework of the SISMOS Project, will be used.

Authors:
Pavel F., Văcăreanu R., Douglas J., Radulian M., Cioflan C., Bărbat A.

Abstract:
The probabilistic seismic hazard analysis for Romania is revisited within the framework of the BIGSEES national research project (http://infp.infp.ro/bigsees/default.htm) financed by the Romanian Ministry of Education and Scientific Research in the period 2012–2016. The scope of this project is to provide a refined description of the seismic action for Romanian sites according to the requirements of Eurocode 8. To this aim, the seismicity of all the sources influencing the Romanian territory is updated based on new data acquired in recent years. The ground-motion models used in the analysis, as well as their corresponding weights, are selected based on the results from several recent papers also published within the framework of the BIGSEES project. The seismic hazard analysis for Romania performed in this study are based on the traditional Cornell-McGuire approach. Finally, the results are discussed and compared with the values obtained in the recently completed SHARE research project. The BIGSEES and SHARE results are not directly comparable since the considered soil conditions are different—actual soil classes for BIGSEES and rock for SHARE. Nevertheless, the analyses of the seismic hazard results for 200 sites in Romania reveal considerable differences between the seismic hazard levels obtained in the present study and the SHARE results and point out the need for further analyses and thorough discussions related to the two seismic hazard models, especially in the light of a possible future harmonized hazard map for Europe.

Authors:
Plăcintă A.O., Popescu E., Borleanu F., Radulian M., Popa M.

Abstract:
The crustal seismicity in Romania is concentrated in front of the Carpathians Arc bend (Vrancea region) and at the contact between the extra-Carpathian platform regions and Carpathians orogen. The region investigated in this paper is characterizing the contact of the western side of the South Carpathians with the Tisza-Dacia region. In this area, the large amount of transcurrent deformation that took place during the right-lateral movement of the South Carpathians in respect to the stable Moesian unit let to the creation of intra-mountainous pull-apart basins able to accommodate this movement. For two such basins, Ha?eg and Caransebe?-Mehadia, recent good quality seismic data have recorded during three earthquake sequences: (1) a sequence of 14 events occurred on 24?31 March 2011 in the Ha?eg Depression (maximum magnitude of Mw = 3.3), (2) a sequence of 35 events occurred on 8?11 September 2013 in the Ha?eg Depression (maximum magnitude of Mw = 4.0) and (3) a sequence of 60 events occurred in the Caransebe?-Mehadia Depression on 31 October?15 December 2014 (main shock magnitude of Mw = 4.1). We apply empirical Green?s functions deconvolution and spectral ratios techniques to determine the source parameters. Despite the relative small size of the events, high-quality waveforms for pairs of co-located events are available in different measuring sites. The new results, together with previous determinations, provide a useful database to investigate the source scaling properties in correlation with seismotectonics modeling of the study region. Finally, source characteristics (location, seismic moment, source dimension, stress drop, focal mechanism, clustering) are discussed in connection with the seismotectonics features at the scale of the entire Carpathians and adjacent extra-Carpathians contact areas.

Authors:
Popa M., Oros E., Dinu C., Radulian M., Borleanu F., Rogozea M., Munteanu I., Neagoe C.

Abstract:
An earthquake swarm of 940 events with ML magnitude between 0.1 and 4.0 and the depth no more than 25 km occurred during three months in the South-Eastern Carpathians foredeep, in an area of around 200 km2, at 27 km north-east of the Galati city. JHD relocation highlights a rupture area steeply dipping down to 15 km depth along a NE-SW alignment. Although the area is known as seismically active, it was for the first time that such a massive sequence was recorded. Specific seismicity alignments and stress field patterns are emphasized and interpreted in terms of geotectonical features of the region. The analysis of the stress associated with the seismic swarm shows a predominant EW compression and NS extension which is compatible with the regional stress regime in the Carpathians foredeep area. The rather small b-slope value of the frequency-magnitude distribution (0.743) for the swarm events in contrast with the value characterizing the regional seismicity (1.890) suggests a significant increase in the local stress accumulation on relatively larger tectonic structures and is in favor of a major tectonic component of the mechanism responsible for generating the swarm.

Authors:
Popa M., Pavel F.

Abstract:
The papers contained in Part II of this volume are devoted to three main subjects, namely: seismicity of Romania, seismic hazard assessment and the evaluation of local soil conditions. A total of 11 papers authored by researchers from several institutions in Romania, as well as from Bulgaria and which cover all the three above-mentioned subjects were accepted for publication and are contained in this chapter. Some very brief abstracts of these papers are given below.

Authors:
Diaconescu M., Oros E., Craiu A.

Abstract:

Authors:
Popescu E., Radulian M., Plăcintă A.O.

Abstract:
The Vrancea seismic nest is a distinctive case of unusually clustered seismicity at intermediate depths. The source scaling properties are essential elements to understand and model the tectonic processes responsible for generating earthquakes in such a confined lithospheric volume. The purpose of the present paper is to investigate the scaling laws for Vrancea earthquakes on the basis of well-defined source parameters. Spectral ratios technique and empirical Green’s function deconvolution are applied to retrieve source parameters. Previous results are combined with new determinations resulting in an enlarged database (298 events), spanning a magnitude interval from Mw ~ 2.4 to Mw ~ 7.7 (1940 major event). The results show for the most of moderate-magnitude earthquakes a relatively simple source time function and source spectrum, compatible with a circular source model with homogeneous rupture process. The scaling of seismic moment with source radius and stress drop appears to be self-similar over the entire magnitude range of the considered data set (3.0 ≤ Mw ≤ 7.7) and matches well the theoretical scaling for source models generally adopted in source studies. Particular high stress drop values, for moderate and large events, indicate fast and efficient rupture processes at different scales, possibly explained by fast running shear melting processes.

Authors:
Rogozea M., Glavcheva R., Radulian M.

Abstract:

Authors:
Rogozea M., Radulian M.

Abstract:

Authors:
Rogozea M., Radulian M., Popa M., Paulescu D., Oros E., Neagoe C.

Abstract:
The macroseismic effects of three major events recorded in historical time (1738, 1802, 1838) are re-evaluated and compared with three major events recorded in the 20th century in the Vrancea subcrustal source (1940, 1977, 1986). The purpose of the paper is to detect characteristic resemblances and differences in the macroseismic distributions among the study earthquakes. They provide important clues in assessing focal depth interval and specific directivity effects of the sources produced in historical times. Certainly, extension of such information to historical earthquakes will contribute essentially to improve the reliability of seismic hazard evaluation.

Authors:
Stancu I., Ghica D., Radulian M.

Abstract:
The Infrasound Ploştina Array (IPLOR) is part of a seismo-acoustic array with 2.5 km aperture, designed and installed in 2009 in the epicentral Vrancea seismogenic area, at the Carpathian Arc bend in Romania. The array belongs to the National Institute for Earth Physics and includes four infrasound stations and seven seismic stations. The purpose of this study is to analyze the ability of Ploştina infrasound array to detect and discriminate accidental chemical explosions located at regional distances. Two recent chemical explosions produced in Cyprus (2011) and in South-eastern Bulgaria (2012) are investigated. The multi-channel correlation algorithm is applied for the identification and characterization of the infrasound signals generated by the two explosive events, as concerns back azimuth, propagation velocity and frequency content. By applying this approach, we prove the efficiency of Ploştina array in identifying and characterizing infrasound signals caused by accidental chemical explosions.

Authors:
Tătaru D., Năstase E., Toma-Dănilă D.

Abstract:

Authors:
Tătaru D., Poiată N., Grecu B., Radulian M., Popa M.

Abstract:
Analysis and characterization of seismicity and its changes is a powerful way to detect, monitor and discriminate between the different types of seismic energy radiations. Modern seismic networks can be today seen as arrays, or antennas, of increasing density and spatial coverage, recording continuous high-quality signals, and making it possible to explore time and frequency scales at which seismic processes were essentially unknown. Seismic activity in Romania covers a wide range of tectonic environments from intermediate depth seismicity in the Vrancea area to the shallow crustal sources, such as those of Dobrogea and Banat. Moreover, Romania is a site of various mining and oil exploitation campaigns. A significant part of seismicity is associated to such industrial contexts as: quarries (Dobrogea, Campulung, Rosia Poieni), dams (Bicaz, Vidraru), mining (Petrosani), or oil exploitations. These kinds of seismic activity have an increasing impact on society. The aim of this study is to present developments towards an integrated framework for detection, location and characterization of seismic sources associated to natural (tectonic) and anthropogenic environments in Romania. We discuss a detection and location methodology based upon most novel developments in the field of seismic source observation that can be applied to a large range of observations, from regular tectonic earthquakes to the micro-seismicity and seismic swarm observations. The performance of the method is tested on a pilot case of the 2013 seismic crises near the city of Galati and the potential fmiher developments and applications are discussed in the light of a more general context.

Authors:
Tătaru D., Toma-Dănilă D., Năstase E.

Abstract:
In order to remain essential cultural and educational institutions, exhibitions and museums need to adapt to the times we live in and to the pace of technology and human interests. Through this paper, we present our own experience and research in developing a state-of-the art earthquake-related exhibition that meets the demands of our times and efficiently addresses a large and diverse target audience. The MOBEE (MOBile Earthquake Exhibition) Project tackles a very problematic topic in regard to the present and future of Romania: the key role of education, in the perspective of a future major earthquake. The project is the only initiative of this kind in Romania, a country where the lessons of previous destructive earthquakes (of 1940 and 1977) seem to be neglected. One of the main goals of the exhibition is to provide a reliable, attractive and- up-to-date source of information regarding earthquakes, leading to mitigation by education. The initiative translates modern approaches into science, arts and computer science into end-products with a direct impact in forming (awakening) and developing the interest for earth science. We provide an insight on how and why new technologies and concepts like large-scale 3D printed maps and models, digital animations and app development, hands-on experiments, or flexible content were put to use. We hope that by sharing our experience we can help and stimulate other similar initiatives and propagate the mobile exhibition concept, as a form of reaching the nowadays audiences (besides the online environment, which we also cover).

Authors:
Tătaru D., Toma-Dănilă D., Năstase E., Zaharia B., Grecu B.

Abstract:
Seismology is a multidisciplinary research domain known as a blend of theoretical and applied research in Earth science and physics, dealing mainly with the fundamental study of earthquakes, seismic waves but also prospecting and recovery of natural resources. Seismology also made possible to look into the deep inaccessible interior of the Earth at depths of up to thousands of kilometers and to extract information about the earthquake parameters and wave propagation and use it to evaluate seismic hazard and risk to buildings, power plants and other infrastructure. And not known by many, seismology was and is used to monitor clandestine nuclear explosions and thus brings a contribution to maintain peace on earth. All the mentions above make seismology a perfect topic to communicate the very essence of science, raise the enthusiasm and excitement of students for scientific discoveries and show the importance of understanding the complexity of our planet - all this knowledge contributing to the building of a more resilient society. Even if, at a first glance, all behind seismology seems to be a quite complicated research, in fact, many fundamental theories and facts can be comprehended from the very first educational grades. That is why, looking backwards, seismology also provides opportunities to teach many science, math and technology concepts and skills to learners of all ages. Unfortunately, as studies have shown, geoscience topics get less and less within the science curriculum, only briefly into geography courses. A change can come from seismology projects that aim to influence the future development of the science curriculum by proving the use of earthquakes and seismology in learning school physics, math and geography. Such a pilot project - entitled Romanian Educational Seismic Network (ROEDUSEIS) has been under implementation for 5 years in more than ten Romanian high schools. Beyond the common objectives and advantages that such a project brought to participating schools (seismometer in the classroom, real time seismic data viewing and processing), we succeeded to propose an interdisciplinary school choice discipline (related to physics, geography & ICT), that is taught in five 11th grade classes, having seismology as a centralizing theme. It comprises lessons on force, friction, wave propagation, and engineering design as well as plate tectonics and driving forces. The role of technology in accessing, processing and using information is underlined through the use of dedicated educational software for detecting, locating and analyzing explosions and earthquakes. For all the other schools we embedded the lessons in existing schools topics rather than creating a new module. In fact, seismology offers unique opportunities to enrich science and physics curriculum and finding creative teachers that are able to deliver innovative lessons, thus improving the chances that students become more interested in science even as a future career path. And thus is a natural transition to another clearly state objective of a seismology education project: to improve the quality of science, technology, engineering and mathematics (STEM) career guidance for students, to help them make informed post16 subject choices.

Authors:
Tătaru D., Zaharia B., Grecu B., Țibu S., Brișan N., Georgescu E.S.

Abstract:
The Romanian Educational Seismic Network project is an educational initiative which launches a challenge for the Romanian educational system: how to use seismology in classrooms for raising awareness on earthquake risk as well as a tool for influencing the development of science curriculum. The project is piloted in nine schools. Educational materials were developed comprising theoretical aspects, activities and experiments related to earthquakes and their effects. First Romanian educational seismic network was built and workshops for teachers were organized with the purpose of showing how Earth Science topics can be taught in classrooms based on the concept “learning by doing”.

Authors:
Tătaru D., Bican-Brisan N., Zaharia B., Grecu B., Toma-Dănilă D., Țibu S.

Abstract:

Authors:
Toma-Dănilă D., Tătaru D.

Abstract:

Authors:
Bălan F.S., Apostol B.F.

Abstract:

Authors:
Bostan D.C., Manea E.F., Ștefan S.

Abstract:
Within this paper the cloudiness spatial and seasonal distribution is analyzed for the eastern part of Romania (Moldavia Region) for a five years period (2006 2010). Hourly data (total and partial cloudiness) from 14 surface observation stations have been used to build a small data base. In order to increase the cloudiness accuracy, an algorithm to derive the partial cloudiness has been applied. This data base allowed us to generate an improved climatology of total and partial cloudiness for Moldavia Region. As an application, the built data base has been used to validate the cloudiness simulated by the mesoscale numerical weather prediction model ALARO. The model results were compared to observation for one year. The obtained statistics have been used to tune the free parameter of the model cloudiness parameterization scheme.

Authors:
Bălă A., Grecu B., Arion C., Popescu E., Toma-Dănilă D.

Abstract:
Different studies focused on the Vrancea subcrustal source of earthquakes pointed out the strong lateral inhomogeneous distribution of the seismic radiation. This implies characteristic macroseismic distributions, extremely elongated along NE-SW direction, and sharply restraint toward NW and SE. Many authors ascribed this particular radiation pattern to the predominant focal mechanism noticed for the major Vrancea shocks [1]. However, a few papers showed that the lateral variation in the subcrustal region seems to be more important (e.g., [2];[3]). We plan in this paper to asses the importance of the source and path of the Vrancea earthquakes on the ground motion parameters in the area of Bucharest. The fault plane solutions of most Vrancea earthquakes indicate a nearly pure thrust mechanism with the B-axis striking NE, which is typical for the strongest events. However there are some earthquakes that do not follow this pattern. We analyze the influence of focal mechanism radiation and source frequency content on the ground motion parameters in Bucharest area. The role of the focal mechanism of the earthquakes and of the depth at which the earthquakes occur determine the path on which seismic waves are propagating to the surface. A significant role is played by the variation of the lithosphere structure between the depth of earthquakes (60-160 km) and the surface, for the seismic motion recorded in the Bucharest area. The analysis of a recent set of intermediate depth earthquakes with Mw > 4.5, for which the focal mechanism have been computed, show the significant role played by the variation of these parameters in respect to the seismic motion recorded in the Bucharest area. These parameters might be in some cases as important as the site effects in establishing the local seismic hazard for the Bucharest City.

Authors:
Ștefan S., Roman I.

Abstract:
The aim of this paper is to analyze the temporal variability of Particulate Matter mass concentrations in connection with air circulation, for eight rural sites situated in the Central and Eastern parts of Europe. The stations from Poland, Hungary and Romania are rural stations without sources of pollutants. The analysis covers four winters, between December 2004 and February 2008. The pollution episodes were selected to explain air circulation influence. The results show that the causes of pollution were local, due to high mean sea level pressure and the blocking, as air circulation on large scale, was dominant in the cases of enhanced pollution in the selected area.

Authors:
Ioane D., Șerban A., Diaconescu M., Chițea F., Caragea I.

Abstract:
A sudden seismological unrest started on mid-September 2013 in the Izvoarele village area, earthquakes and subterranean noises occurring almost continuously for a month. The seismological monitoring provided more than 370 seismic events, with magnitude ranging between 0.3 and 4.0 and depth ranging from 0.3 km to more than 30 km. Considering the historical seismicity, studied during the end of the XIXth century and the first half of the XXth century by means of seismic intensity, the Izvoarele-Galati area represents the southern end of a N-S high seismicity sector developed between Barlad and Galati. Based on these observations regarding epicentral areas and destructive effects, several NW-SE to N-S trending lines of "seismic sensitivity" were interpreted at that time. The study of the 2013 seismic sequence showed that most earthquakes provided magnitudes between 0.3 and 1.5, ca 10% having higher magnitudes (16 more than 2.5, 11 more than 3.0 and 8 more than 3.5). The relationship between Magnitude and Depth for the recorded seismic events displays a scattered distribution of the 2013 seismic events with low magnitude values (0.3 to 2.0), most of them included in the 0.1-10.0 km depth interval. Higher magnitude earthquakes (2.0 to 4.0) were generated in a smaller range of depth values (3.0 to 7.0). The relationship between Magnitude and Time illustrates three main stages of high seismicity for the studied 2013 seismological event: September 25-27, September 30 to October 7 and October 12-15, with exceptionally dense seismic activity during October 2-5. Considering the spatial development of the active seismic zone, two parallel lines trending NE-SW in the area were observed when plotting the earthquakes epicentres with magnitude higher than 3.0. Active segments of a regional NE-SW trending fault system were interpreted this way. The seismic events that occurred at depths higher than 10 km illustrated several distinct episodes during the intense seismological activity: September 23 and 28-29; October 4-5, 15 and 20-21. A quite close spatial association was found between the 2013 high seismicity area and an oil exploitation facility, the extracting works dating here from the second half of the XXth century. The oil reservoirs are shallow, located between 0.5 and 0.7 km depth, the sandy deposits being sealed by faults or compact crystalline rocks. Induced seismicity might be expected as brine is being injected during time to replace the extracted oil. A characteristic of this geological structure, that might be important in understanding the unusual seismicity and subterranean noises, is represented by the thin marl beds separating the sandy beds, which collapse in case of a sudden pressure decrease and determine the flooding of the oil reservoir.

Authors:
Mărmureanu A., Craiu G., Craiu A., Rădulescu S, Neagoe C., Ionescu C.

Abstract:
Providing warning notification several seconds before dangerous earthquake waves arrive at a target site reduces the property damages and human casualties. Most earthquake early warning systems (EEWS) developed are either regional (“network based”) or on-site (“stand alone”) systems. The recent upgrade of the seismic network in Romania with high dynamic range accelerometers allows recording of moderate to large magnitude earthquakes at very close epicentral distances (less than 10–20 km). This allows an increase of the warning lead-time (the time difference between the alert notification time and the arrival time of potentially destructive waves at a given target). The seismicity of Romania is significantly affected by earthquakes produced by the Vrancea seismic source with intermediate depth events (three shocks/century with magnitude Mw greater than 7.0). In this paper we present the performance of the seismic network in rapidly locate events occurring in the Vrancea area. Since rapid location of earthquakes is the first step in issuing early warning notifications, by reducing the time of the first valid location will lead to an increase the lead-time interval. Also rapid location of events will allow a future upgrade of EEWS to cover the entire Romanian territory.

Authors:
Pavel F., Văcăreanu R., Radulian M., Cioflan C.O.

Abstract:
This paper evaluates possible directional effects from strong ground motions recorded during the last four significant subcrustal earthquakes produced in the Vrancea seismic zone (Romania) in August 1986 (M (W) = 7.1), May 1990 (M (W) = 6.9 and 6.4) and October 2004 (M (W) = 6.0). Several measures of the horizontal component of the ground motion given in the literature (Boore et al., 2006; Boore, 2010) are computed and are related to the geometric mean of the as-recorded horizontal components. ANOVA method is applied in order to quantify the influence of the earthquake magnitude and of the soil class on some strong ground motion parameters (e.g. Arias intensity, PGV/PGA, or mean period T (M)). The study of the directional effects is performed using the distribution of I (JMA) and of the rotation angle corresponding to a measure of the horizontal component of the ground motion (RotD100) and the results reveal a visible directional pattern for I (JMA), while in the case of RotD100 the directional patterns are less visible.

Authors:
Văcăreanu R., Radulian M., Iancovici M., Pavel F., Neagu C.

Abstract:
A next generation ground motion model for the prediction of spectral accelerations both in the fore-arc and back-arc regions of the Carpathians Mountains is developed in this research for the Vrancea intermediate depth seismic source in Romania. This ground motion prediction equation (GMPE) is an updated version of the model given in Vacareanu et al. [2014] and is applicable in both the fore-arc and the back-arc regions. The strong ground motion database from which the prediction model is derived consists of over 700 triaxial accelerograms from Vrancea subcrustal seismic events, as well as from other intermediate-depth earthquakes produced in other seismically active regions in the world. The applicability of this ground motion prediction model in both the fore-arc and the back-arc region is tested using the analysis of residuals. Moreover, the appropriateness of this GMPE for soil classes B and C defined in EN 1998-1, as well as for average soil conditions is investigated. All results suggest that this model is an improvement of the previous versions of ground motion prediction equations for Vrancea intermediate-depth seismic source and its use in both the fore-arc and the back-arc regions make it a reliable candidate for more accurate seismic hazard studies of Romania.

Authors:
Maggipinto T., Biagi P.F., Colella R., Schiavulli L., Ligonzo T., Ermini A., Martinelli G., Moldovan I.A., Silva H., Contadakis M., Skeberis C., Zaharis Z., Scordilis E., Katzis K., Buyuksarac A. and D’Amico S.

Abstract:
On October 12, 2013, an earthquake with Mw = 6.5 occurred in the southern Hellenic Arc, approximately 20 km off the west coast of Crete. The main shock, the focal depth of which is on the order of 40 km, was followed by aftershocks felt in the nearby cities and villages, although the aftershock sequence was poor. The epicentre was located at approximately 60 km from a radio receiver in Crete (CRE), which belongs to the European VLF/LF Radio Network. Several days before the earthquake, a clear disturbance occurred in one of the ten radio signals that the CRE receiver sampled. The disturbance, which can be considered an anomaly, appeared in the 216 kHz radio signal radiated by the Radio Monte Carlo (MCO) transmitter. The radio path MCO-CRE crossed directly over the epicentre area of the aforementioned earthquake. In this work, we present a detailed analysis of the MCO signal anomaly using spectral tools. We also investigate the behaviour of other radio signals sampled by the CRE receiver and consider other possible causes of disturbances on the MCO radio signal. We conclude that the disturbance in the MCO radio signal is a convincingly possible precursor of the earthquake in Crete. Emission of electromagnetic waves with a frequency band that includes 216 kHz from the focal zone of the earthquake can provide a satisfactory explanation of the radio anomaly.

Authors:
Dolea P., Cristea O., Dascal P.V., Moldovan I.A., Biagi P.F.

Abstract:
In the last decades, one of the main research directions in identifying seismic precursors involved monitoring VLF (Very Low Frequency) and LF (Low Frequency) radio waves and analysing their propagation characteristics. Essentially this method consists of monitoring different available VLF and LF transmitters from long distance reception points. The received signal has two major components: the ground wave and the sky wave, where the sky wave propagates by reflection on the lower layers of the ionosphere. It is assumed that before and during major earthquakes, unusual changes may occur in the lower layers of the ionosphere, such as the modification of the charged particles number density and the altitude of the reflection zone. Therefore, these unusual changes in the ionosphere may generate unusual variations in the received signal level...

Authors:
Pavel F., Văcăreanu R., Douglas J., Radulian M., Cioflan C.O., Barbat A.

Abstract:
The probabilistic seismic hazard analysis for Romania is revisited within the framework of the BIGSEES national research project (http://infp.infp.ro/bigsees/default.htm) financed by the Romanian Ministry of Education and Scientific Research in the period 2012–2016. The scope of this project is to provide a refined description of the seismic action for Romanian sites according to the requirements of Eurocode 8. To this aim, the seismicity of all the sources influencing the Romanian territory is updated based on new data acquired in recent years. The ground-motion models used in the analysis, as well as their corresponding weights, are selected based on the results from several recent papers also published within the framework of the BIGSEES project. The seismic hazard analysis for Romania performed in this study are based on the traditional Cornell-McGuire approach. Finally, the results are discussed and compared with the values obtained in the recently completed SHARE research project. The BIGSEES and SHARE results are not directly comparable since the considered soil conditions are different—actual soil classes for BIGSEES and rock for SHARE. Nevertheless, the analyses of the seismic hazard results for 200 sites in Romania reveal considerable differences between the seismic hazard levels obtained in the present study and the SHARE results and point out the need for further analyses and thorough discussions related to the two seismic hazard models, especially in the light of a possible future harmonized hazard map for Europe.

Authors:
Toma-Dănilă D., Zulfikar C., Manea E.F., Cioflan C.O.

Abstract:
Bucharest, capital of Romania, is one of the most exposed big cities in Europe to seismic damage, due to the intermediate-depth earthquakes in the Vrancea region, to the vulnerable building stock and local soil conditions. This paper tries to answer very important questions related to the seismic risk at city scale that were not yet adequately answered. First, we analyze and highlight the bottlenecks of previous risk-related studies. Based on new researches in the hazard of Bucharest (recent microzonation map and groundmotion prediction equations, reprocessed real recorded data) and in vulnerability assessment (analytical methods, earthquake loss estimation software like SELENA and ELER, the recently implemented Near Real-Time System for Estimating the Seismic Damage in Romania) we provide an improved estimation of the number of buildings and population that could be affected, for different earthquake scenarios. A new method for enhancing the spatial resolution of the building stock data is used successfully. (C) 2015 Elsevier Ltd. All rights reserved.

Authors:
Moldovan I.A., Constantin A.P., Biagi P.F., Toma-Dănilă D., Moldovan A.S., Dolea P., Toader V.E., Maggipinto T.

Abstract:
The Romanian VLF / LF monitoring system consists in a radio receiver and the infrastructure that is necessary to record and transmit the collected data, and is part of the international initiative INFREP and was put into operation in December 2009 on the Black-Sea shore (Dobruja Seismologic Observatory - Dob-RO). Since then the system was developed by replacing the vertical antenna with a magnetic loop-type one, by installing a vertical electric field monitor and a weather station, and by designing special software for the transfer, storage and initial processing of data using the LabView software platform.

Authors:
Bălă A., Grecu B., Arion C., Popescu E., Toma-Dănilă D.

Abstract:
Providing warning notification several seconds before dangerous earthquake waves arrive at a target site reduces the property damages and human casualties. Most earthquake early warning systems (EEWS) developed are either regional ("network based") or on-site ("stand alone") systems. The recent upgrade of the seismic network in Romania with high dynamic range accelerometers allows recording of moderate to large magnitude earthquakes at very close epicentral distances (less than 10-20 km). This allows an increase of the warning lead-time (the time difference between the alert notification time and the arrival time of potentially destructive waves at a given target). The seismicity of Romania is significantly affected by earthquakes produced by the Vrancea seismic source with intermediate depth events (three shocks/century with magnitude Mw greater than 7.0). In this paper we present the performance of the seismic network in rapidly locate events occurring in the Vrancea area. Since rapid location of earthquakes is the first step in issuing early warning notifications, by reducing the time of the first valid location will lead to an increase the lead-time interval. Also rapid location of events will allow a future upgrade of EEWS to cover the entire Romanian territory.

Authors:
Bălă A., Răileanu V., C. Dinu, M. Diaconescu

Abstract:
The most significant seismicity in Romania is located in a relatively small area-the Vrancea seismogenic zone, where 2-3 intermediate depth strong earthquakes (Mw>7.0) occur in a century. Although the crustal seismicity is dispersed in several zones of country, only in a few areas the observed magnitudes exceeded Mw=6.0. Nevertheless some crustal earthquakes that occurred in the past have resulted in damages and even casualties. These facts imposed the taking into account of crustal seismicity in the seismic hazard mapping. Crustal seismicity in Romania is distributed within some belts located along of Carpathians and the Pannonian depression having a more significant concentration in the Vrancea crustal area and in the front of Eastern Carpathians bend, in the Fagaras Mountain area, in the Danubian area, Banat, Crisana, Maramures and North Dobrogea regions. A summary of the crustal seismic activity beneath the western part of Romanian is presented pointing out the most significant events known from both historical and instrumental records. The observed crustal seismicity did not exceed Mw= 5.6 excepting the Fagaras area where the strongest events reached up to Mw=6.5. For each crustal seismogenic zone the main fault systems which can account for the local seismicity are presented. This study presents a correlation of seismicity data with the local tectonics. Special attention is focused on the Transylvanian Basin and on the Pannonian sector where a correlation of seismicity with deep structure is better documented.

Authors:
Craiu A., Mărmureanu A., Diaconescu M., Craiu M.G., Ionescu C.

Abstract:
In this paper we present the results obtained during the study of swarm of earthquake close to the Galati city. In the last period the National Seismic Network was continuously upgraded, which allows presently to easily detect earthquakes with very low magnitudes in every seismic region of Romania. The seismogenic region of the swarm is situated between two main crustal faults, oriented SE-NW: Sf. Gheorghe fault (located in North Dobrogea, in the Scythian Platform) to the North, and Peceneaga Camena fault (which separates North Dobrogea block from the Moesian Platform) to the South. The epicentral zone belongs to a complex tectonic area, in which a secondary fault system – lying NE-SW, perpendicular to the dominant system – is present too. The seismic swarm started on September 23, 2013, close to Galati city, in Izvoarele region (Romania), and lasted until November 12, 2013. 406 earthquakes were recorded during several phases of seismic activity. The strongest events – a magnitude 3.9 earthquake, occurred on September 29, and two ML 3.8 shocks, which occurred on October 3 and October 4, respectively, were accompanied by specific seismicity bursts. The spatial distribution of the epicenters, which are aligned in NE-SW direction, indicates that the seismic swarm was generated by the second fault system. The focal mechanisms show normal slip, with one of the nodal planes oriented roughly in NE-SW direction. The results are discussed and interpreted in relation with the regional seismotectonics, our study aiming to emphasize new elements and implications for seismic hazard evaluation in the Galati area. Key word: seismic swarm, focal mechanism

Authors:
Craiu A., Craiu M.G., Diaconescu M., Mărmureanu A.

Abstract:
The systematic studies of the focal mechanism solutions furnish fundamental data about some of the main factors that control the seismic phenomenon, e.g. stress field peculiarities and the types of faulting, the geometry of the faults and provide critical information for global, regional and local tectonic studies, as well as for many types of seismological investigations. In the last few years were recorded some significant earthquakes in the Vrancea subcrustal domain and in other seismic regions at crustal depths. The National Seismic Network was continuously updated in the last years and now the recordings of these events contribute to a complete database and are very important to seismology and seismic hazard assessment studies. The substantial increase in the seismic recordings and the azimuthal gap leads to a more precise knowledge of focal mechanism, structure and source parameters. The seismicity of Romania is distributed in several epicentral zones: Vrancea, Fagaras-Campulung, Banat, Crisana, Maramures, and Dobrogea. The main goal of this paper is to study seismicity evolution and the focal mechanism analysis of recent earthquakes occurred in Romania (in last five years) and their correlation with the average stress field. We have determined fault plane solutions and analyzed the seismic activity recorded on the Romania territory in connection with seismogenic zones. At the same time, our results are integrated and interpreted in connection with the stress field characteristics, deduced from the available fault plane solutions on different depth intervals.

Authors:
Craiu M.G., Mărmureanu A., Craiu A., Ionescu C.

Abstract:

Authors:
Diaconescu M., Craiu A., Toma-Dănilă D.

Abstract:
Earthquakes from the Fagaras seismic zone originate in the Southern Carpathians area and they have foci located East and West of the OLT Valley. In this area the largest earthquake occurred after the Vrancea area on 26.01.1916, with an intensity estimated to have exceeded level 7 in the epicenter (Mw= 6.4), which was followed by numerous aftershocks extended about 6 months. On the same day as the main earthquake of 6.4 (Mw) also produced other three quakes one of 5.2 (Mw), one of 5 (Mw), and one of 4.4 (M-W). The series of earthquakes in 1916 appears to be due not to an outbreak not only, but tectonic movements along a line on the alignment Băbuieşti-Confluence-Piscu Negru. Other seismic lines are: Călimăneşti- Coteşti-Horezu and Arefu-Ismailia-Govora where I <5 degrees.The earthquakes from the 1916 seismic sequence have shifted from North-West to South-East. Earthquakes have occurred in the south have North West direction on deep fractures following hercinic ages, and the Northeast directions of the Alpine age. The fault plane solutions of some more recent earthquakes showed a shear mechanism through compression and are associated with the deep faults oriented W-E or N-S, faults associated with the thrust of the Supragetic domain over the Getic domain. Note that the total of 474 events recorded between 1550 and 2014, 13 earthquakes were generated before 1900 and have the largest magnitudes (5 of them have the magnitude 6.2

Authors:
Ioane D., Șerban A., Diaconescu M., Chițea F., Caragea I.

Abstract:
A sudden seismological unrest started on mid-September 2013 in the Izvoarele village area, earthquakes and subterranean noises occurring almost continuously for a month. The seismological monitoring provided more than 370 seismic events, with magnitude ranging between 0.3 and 4.0 and depth ranging from 0.3 km to more than 30 km. Considering the historical seismicity, studied during the end of the XIX th century and the first half of the XX th century by means of seismic intensity, the Izvoarele–Galati area represents the southern end of a N-S high seismicity sector developed between Barlad and Galati. Based on these observations regarding epicentral areas and destructive effects, several NW-SE to N-S trending lines of " seismic sensitivity " were interpreted at that time. The study of the 2013 seismic sequence showed that most earthquakes provided magnitudes between 0.3 and 1.5, ca 10% having higher magnitudes (16 more than 2.5, 11 more than 3.0 and 8 more than 3.5). The relationship between Magnitude and Depth for the recorded seismic events displays a scattered distribution of the 2013 seismic events with low magnitude values (0.3 to 2.0), most of them included in the 0.1–10.0 km depth interval. Higher magnitude earthquakes (2.0 to 4.0) were generated in a smaller range of depth values (3.0 to 7.0). The relationship between Magnitude and Time illustrates three main stages of high seismicity for the studied 2013 seismological event: September 25-27, September 30 to October 7 and October 12-15, with exceptionally dense seismic activity during October 2-5. Considering the spatial development of the active seismic zone, two parallel lines trending NE-SW in the area were observed when plotting the earthquakes epicentres

Authors:
Mărmureanu A., Ionescu C., Craiu M.G., Craiu A., Tolea A.

Abstract:

Authors:
Tătaru D., Grecu B., Zaharia B., Toma-Dănilă D., Năstase

Abstract:
The Carpathian seismic belt (Vrancea Area), located in Romania, is one of the most active tectonic regions in Europe. In the last few decades, the country has experienced several major earthquakes which have claimed thousands of lives and caused significant economical damage (Vrancea, 1940; 1977; 1986). Even so, little is currently done for the general public in order to mitigate the possible effects of a future major earthquake. As intermediate depth earthquakes affect a vast area (up to 400 km from the epicenter), there is a continuous need in raising awareness by sharing information and knowledge in a broader area and to a larger audience. To have a proper framework for engaging new communities and build partnerships, with benefit for all parties involved, a series of pilot projects have been initiated by National Institute for Earth Physics (NIEP) researchers. Here we will focus on just two of them, named by their acronym: ROEDUSEIS and MOBEE. Improving public awareness and education of population is an essential part of mitigating the natural risks. Starting this effort at the level of schools and opening the doors for the wide public to take part, will certainly be a way to increase the chances of success. Our view is that the research institutes should have a leading role in providing useful data regarding the earthquakes, thus helping the better understanding of this natural phenomenon, and thus bringing its contribution to build a more resilient society.

Authors:
Tătaru D., Grecu B., Zaharia B., Oros E., Bălă A.

Abstract:
As a result of the deployment of the permanent Romanian broadband stations in the last 10 years, valuable data for seismicity and crustal structure studies in Romania has become available. Complementary to this dataset, during a joint project between University of Leeds, UK and National Institute for Earth Physics, Romania (South Carpathian Project – SCP), 33 broadband seismic stations autonomously operated in the western part of the country and continuously provided data for two years (2009-2011). This project offered a good opportunity to study the seismicity and structure of western Romania. First, we study the spatial distribution of epicenters and temporal distribution of origin times of the events occurred between July 2009 and June 2011 and we show that many of the seismic events grouped into clusters are of artificial origin. We also investigate the background seismic noise at stations deployed during SCP experiment and notable diurnal and seasonal variations have been observed at most of the stations. Finally, we used the receiver function technique and a joint inversion technique of receiver function and Rayleigh wave dispersion to derive velocity models for each seismic station location. The results show a thin crust for stations located inside the Pannonian basin (28-30 km). The stations within the Southern and Central Carpathian Orogen are characterized by crustal depths of ~35 km. For two station located in the Apuseni Mountains the Moho discontinuity is replace by a transition zone extended between 36 to 40 km depth.

Authors:
Ivan M., Ghica D.V., Gosar A., Hatzidimitriou P., Hofstetter R., Polat G., Wang R.J.

Abstract:
Lowermost mantle velocity in the area 15A degrees S-70A degrees N latitude/60A degrees W-5A degrees W longitude is estimated using two groups of observations, complementary to each other. There are 894 Pdif observations at stations in the Balkan and Eastern Mediterranean areas from 15 major earthquakes in Central and South America. Another 218 Pdif observations are associated with four earthquakes in Greece/Turkey and one event in Africa, recorded by American stations. A Pdif slowness tomographic approach of the structures immediately above the core-to-mantle boundary (CMB) is used, incorporating corrections for ellipticity, station elevation and velocity perturbations along the ray path. A low-velocity zone above CMB with a large geographical extent, approximately in the area (35-65A degrees N) x (40-20A degrees W), appears to have the velocity perturbations exceeding the value actually assumed by some global models. Most likely, it is extended beneath western Africa. A high-velocity area is observed west of the low-velocity zone. The results suggest that both Cape Verde and Azorean islands are located near transition areas from low-to-high velocity values in the lowermost mantle.

Authors:
Mărmureanu G., Mărmureanu A., Cioflan C.O.

Abstract:
The nonlinear seismology is the rule, The linear seismology is the exception. Paraphrasing Tullio Levi-Civita The leading question is: how many cities, villages, metropolitan areas etc. in seismic regions are constructed on rock sites? Most of them are located on alluvial deposits/ sediments, on Quaternary layers or in river valleys. In last book written by Peter M. Shearer, Professor of Geophysics at University of California, we can find, in total, only 12 rows about non-linear seismology(page 176).Among others are the following conclusions:(i)-Strong ground accelerations from large earthquakes can produce a non-linear response in shallow soils; (ii)-When a non-linear site response is present, then the shaking from large earthquakes cannot be predicted by simple scaling of records from small earthquakes; (iii)-This is an active area of research in strong motion and engineering seismology. On the other hand, Aki wrote: Nonlinear amplification at sediments sites appears to be more pervasive than seismologists used to think…Any attempt at seismic zonation must take into account the local site condition and this nonlinear amplification(Aki, A., Local Site Effects on Weak and Strong Ground Motion, Tectonophysics,218,93-111,1993). The difficulty to seismologists in demonstrating the nonlinear site effects has been due to the effect being overshadowed by the overall patterns of shock generation and propagation. In other words, the seismological detection of the nonlinear site effects requires a simultaneous understanding and separating of the effects of earthquake source, propagation path and local geological site conditions. To see the actual influence of nonlinearity of the whole system (seismic source-path propagation-local geological structure) the authors used to study the response spectra because they are the last in this chain and, of course, that they are the ones who are taken into account in seismic design of all structures Stress-strain relationships for soils are usually nonlinear, soil stiffness decreases and internal damping increases with increasing shear strain during of strong earthquakes. There is a strong nonlinear dependence of the spectral amplification factors(SAF) on earthquake magnitude for all seismic stations on Romanian territory on extra-Carpathian area (Iasi, Bacau, Focsani, Bucharest etc.). Median values of SAF for last strong Vrancea earthquakes are decreasing from 4.16(May 31,1990;Mw=6.4),to 3.63 (May 30,1990;Mw=6.9) and to 3.26 (August 30, 1986; Mw=7.1) .The novelty and the complexity degree comes from the fact that for first time, the final decision for NPP Cernavoda site was also based on local strong nonlinear spectral amplifications for strong earthquakes and used in last "STRESS TEST" asked by IAEA Vienna in 2011. The present analysis indicates that the effect of nonlinearity could be very important and if the analysis is made for peak accelerations, it is 48.87% and for stronger earthquakes it will be bigger. The authors are coming with new recorded data which will open up a new challenge for seismologists studying nonlinear site effects in 2-D and 3-D irregular geological structures, leading them to a fascinating research subject in earth physics(Aki,1993, p.108,idem),in nonlinear seismology and,finally, in a real evaluation of earthquake risk and loss estimates.

Authors:
Moldovan I.A., Constantin A.P., Biagi P.F., Toma-Dănilă D., Moldovan A.S., Dolea P., Toader V.E., Maggipinto T.

Abstract:
The Romanian VLF / LF monitoring system consists of a radio receiver and the infrastructure that is necessary to record and transmit the collected data, and is part of the international initiative INFREP and was put into operation in December 2009 on the Black-Sea shore (Dobruja Seismologic Observatory – Dob-RO). Since then the system was developed by replacing the vertical antenna with a magnetic loop-type one, by installing a vertical electric field monitor and a weather station, and by designing special software for the transfer, storage, and initial processing of data using the LabView software platform.

Authors:
Oikonomou C., Toma-Dănilă D., Haralambous H., Muntean A., Moldovan I.A.

Abstract:
We examine the lithosphere-atmosphere-ionosphere interaction with respect to earthquake events using Total Electron Content (TEC) data deriving from the Romanian permanent GPS network by applying three different techniques: a) estimation of TEC deviations from the mean state, b) Cross-Correlation Analysis and c) Spectral Analysis. The analysis concerns four seismic events that took place in Romania with magnitude ranging from 5.2 to 6.0. The aim is to identify and study possible ionospheric precursory phenomena linked to these seismic events.

Authors:
Toader, V.E., Moldovan I.A., Ionescu C.

Abstract:
The paper describes a complex multidisciplinary monitoring system designed for Vrancea seismic area (bending area of Carpathians Mountains). This includes hardware (stations with sensors, acquisition and communication equipment) and software for data processing in real time. The result of this work is the growth of an alert service through: perfecting risk evaluation, seismic and climate forecast, informing the decision factors regarding the impact minimization of natural disasters and the education of the population. The information from database will help the scientists to develop the system and to improve their knowledge for other applications. A monitoring network involves a multidisciplinary activity that highlights the interdependence of environmental factors (air, earth) and their balance under normal conditions. Weather or seismic events represent the point of maximum imbalance. Electromagnetic, infrasound, seismoacoustic at high frequencies, air ionization and solar radiation monitoring, in correlation with global and local environmental factors (including seismic zones), is a new approach for atmospheric study in our area. Figure 1 describes a global structure of system. Data are acquired from ground (National Institute for Earth Physics - NIEP seismic stations) and satellites.

Authors:
Bălă A., Răileanu V., Dinu C., Diaconescu M.

Abstract:
The most significant seismicity in Romania is located in a relatively small area - the Vrancea seismogenic zone, where 2-3 intermediate depth strong earthquakes (Mw > 7.0) occur in a century. Although the crustal seismicity is dispersed in several zones of country, only in a few areas the observed magnitudes exceeded Mw = 6.0. Nevertheless some crustal earthquakes that occurred in the past have resulted in damages and even casualties. These facts imposed the taking into account of crustal seismicity in the seismic hazard mapping. Crustal seismicity in Romania is distributed within some belts located along of Carpathians and the Pannonian depression having a more significant concentration in the Vrancea crustal area and in the front of Eastern Carpathians bend, in the Fagaras Mountain area, in the Danubian area, Banat, Crisana, Maramures and North Dobrogea regions. A summary on the crustal seismic activity beneath the Romanian is presented pointing out the most significant events known from both historical and instrumental records. The observed crustal seismicity did not exceed M-w = 5.6 excepting the Fagaras area where the strongest events reached up to M-w = 6.5. For each crustal seismogenic zone the main fault systems which can account for the local seismicity are presented. This study presents a correlation of seismicity data with the local tectonics. A special attention is focused on foreland of the Carpathian orogen and on the Pannonian sector where a correlation of seismicity with deep structure is better documented.

Authors:
Stancu I., Ghica D., Radulian M., Ionescu C.

Abstract:
The Infrasound Plostina Array (IPLOR) is an acoustic array of 2.5 km aperture designed and installed in 2009 in the epicentral Vrancea seismogenic area, at the Carpathian Arc bend in Romania. The Network belongs to the National Institute for Earth Physics (NIEP) and includes 4 infrasound stations and 7 seismic stations. The goal of the present study is to analyze the capacity of the infrasound array of Plostina (Romania) to detect and discriminate quarry blasts from local earthquakes. More than 50% of the shallow seismicity annually recorded in Romania is coming from industrial blasts. Plostina network description and signal processing procedures are discussed in Section 2, Data and Methods. The results of this study are presented in Section 3, and the final discussions conclusions in the end.

Authors:
Stancu I., Ghica D., Radulian M.

Abstract:
Volcanic eruptions represent excellent calibration sources for the IMS infrasound network. The location is precisely known, and the energy released during explosive eruptions may be large enough to generate infrasound waves propagated thousands of kilometers. The purpose of this study is to analyze the network capacity of infrasound from Plostina (Romania) to detect volcanic eruptions. The description of the Plostina network and signal processing procedures are discussed in Section 2, data and methods. The results and discussion of this study are presented in Section 3 and the conclusions at the end.

Authors:
Toader V. E., Popescu I., Moldovan I. A., Ionescu C.

Abstract:
Vrancea's seismicity (Curvature Carpathian mountains) recorded in 2013 an energy discontinuity preceded by the highest seismic inactivity according to the Romanian National Institute for Earth Physics. The energy is calculated based on the local magnitude (Richter), and is cumulative. Vrancea is the most important seismic region from Eastern Europe through its intermediate depth earthquakes. Energy variations can be linearly approximated due to the constant rate of earthquake occurrences. This allows to forecast the magnitude using the inverse energy-magnitude relationship. Periods longer than 5-8 days without earthquakes are followed by a more intense seismic activity. This paper analyses the evolution of seismicity in several Romanian regions that have similar energy deviations. The analysis was performed using a software tool developed by the authors of this paper. Energy discontinuity can be precursors to earthquakes greater than 7R. The analysis used information from NIEP and the European-Mediterranean Seismological Centre (EMSC) database.

Authors:
Mărmureanu G., Cioflan C.O., Mărmureanu A., Ionescu C., Manea E.F.

Abstract:
In seismic hazard evaluation and risk mitigation, there are many random and epistemic uncertainties. On the another hand, the researches in this area as part of knowledge are with rest, that is, the results are with interpretable questions with open answers. The knowledge cannot be exhausted by results. The authors developed in last time the concept of “Nonlinear Seismology – The Seismology of the XXI Century” (Marmureanu et al. Nonlinear seismology-the seismology of XXI century. In: Modern seismology perspectives, vol 105. Springer, New York, pp 49–70, 2005). The leading question is: how many cities, villages, metropolitan areas, etc., in seismic regions are constructed on rock? Most of them are located on soil deposits. A soil is of basic type sand or gravel (termed coarse soils), silt or clay (termed fine soils), etc. Strong ground accelerations from large earthquakes can produce a nonlinear response in shallow soils. This can be studied by comparing surface and borehole seismic records for earthquakes of different sizes. When a nonlinear site response is present, then the shaking from large earthquakes cannot be predicted by simple scaling of records from small earthquakes (Shearer, Introduction to seismology, 2nd edn. Cambridge University Press, Cambridge, 2009). Nonlinear amplification at sediments sites appears to be more pervasive than seismologists used to think…Any attempt at seismic zonation must take into account the local site condition and this nonlinear amplification (Aki, Tectonophysics 218:93–111, 1993). The difficulty for seismologists is to demonstrate the nonlinear site effects, these being overshadowed by the overall patterns of shock generation and propagation. In other words, the seismological detection of the nonlinear site effects requires a simultaneous understanding/knowledge of earthquake source, propagation path, and local geological site conditions. To see the actual influence of nonlinearity of the whole system (seismic source-path propagation-local geological structure), the authors used to study the free field response spectra which are the last in this chain and are taken into account in seismic design of all structures. Soils from the local geological structure at the recording site exhibit a strong nonlinear behavior under cyclic loading conditions and although they have many common mechanical properties, the use of different models to describe their seismic behavior is required. The studies made by the authors in this chapter show that using real spectral amplification factors (SAF), amplifications showing local effects, have values which differ totally from those of crustal earthquakes. The spectral amplifications highlight strong nonlinear response of soil composed of fractured limestone, limestone with clay, marl, sands, clay, etc., and these amplifications are strongly dependent of earthquake magnitude and nature of soils from site. Finally, these amplifiers are compared to those from Regulatory Guide 1.60 of the U. S. Atomic Energy Commission (Design response spectra for seismic design of nuclear power plants. Regulatory Guide 1.60. Rev. 1, Washington, D.C., 1973) which can be used only for crustal earthquakes and not for deep and strong Vrancea earthquakes from Romania. The study of the nonlinear behavior of soils during strong earthquakes may clarify uncertainties in ground motion prediction equations used by probabilistic and classical deterministic seismic hazard analysis.

Authors:
Maggipinto T., Biagi P.F., Colella R., Schiavulli L., Ligonzo T., Ermini A., Martinelli G., Moldovan I.A., Silva H., Contadakis M., Skeberis C., Zaharis Z., Scordilis E., Katzis K., Buyuksarac A., D’Amico S.

Abstract:
On October 12, 2013, an earthquake with M-w = 6.5 occurred in the southern Hellenic Arc, approximately 20 km off the west coast of Crete. The main shock, the focal depth of which is on the order of 40 km, was followed by aftershocks felt in the nearby cities and villages, although the aftershock sequence was poor. The epicentre was located at approximately 60 km from a radio receiver in Crete (CRE), which belongs to the European VLF/LF Radio Network. Several days before the earthquake, a clear disturbance occurred in one of the ten radio signals that the CRE receiver sampled. The disturbance, which can be considered an anomaly, appeared in the 216 kHz radio signal radiated by the Radio Monte Carlo (MCO) transmitter. The radio path MCO-CRE crossed directly over the epicenter area of the aforementioned earthquake. In this work, we present a detailed analysis of the MCO signal anomaly using spectral tools. We also investigate the behavior of other radio signals sampled by the CRE receiver and consider other possible causes of disturbances on the MCO radio signal. We conclude that the disturbance in the MCO radio signal is a convincingly possible precursor of the earthquake in Crete. Emission of electromagnetic waves with a frequency band that includes 216 kHz from the focal zone of the earthquake can provide a satisfactory explanation of the radio anomaly.

Authors:
Ionescu C., Marmureanu A., Marmureanu G., Solakov D., Simeonova S., Dimitrova L.

Abstract:
Providing earthquake warning notifications several seconds before dangerous earthquake waves arrive at a target site significantly reduces the property damages and the number of lives lost. Most earthquake early warning systems (EEWS) developed so far are either regional ("network-based) or "on-site" (stand-alone) systems. The recent upgrade of the seismic networks in Romania and Bulgaria with high dynamic range accelerometers allows recording of moderate-to-large magnitude earthquakes at very close epicentral distances (less than 10-20 km). This allows an increase of the early warning lead-time (the time difference between the alert notification time and the arrival time of potentially destructive waves at a given target). The Romania-Bulgaria border region is significantly affected by earthquakes occurred in both territories: on the one hand, produced by the Vrancea seismic source, with intermediate-depth events (3 shocks/century with magnitude greater than 7), and on the other hand, crustal seismicity recorded in the northern part of Bulgaria (Shabla, Dulovo, Gorna Orjahovitza). In this paper we present the rapid early warning system (REWS) for earthquakes that may affect the border areas of Romania and Bulgaria together with the software tools developed that are now used by emergency situations units in both Romania and Bulgaria.

Authors:
Apostol B.F.

Abstract:
We investigate the effect of the surface inhomogeneities (defects) on the propagation of the elastic waves in a semi-infinite isotropic solid body (half-space). A perturbation-theoretical scheme is devised for small surface defects (in comparison with the relevant elastic disturbances propagating in the body), and the elastic waves equations are solved in the first-order approximation. It is shown that surface defects generate both scattered waves localized (and propagating only) on the surface (two-dimensional waves) and scattered waves reflected back in the body. Directional effects, wave slowness and attenuation by diffusive scattering, or possible resonance effects are discussed.

Authors:
Văcăreanu R., Mărmureanu G., Pavel F., Neagu C., Cioflan C.O., Aldea A.

Abstract:
A strong-ground motion database of more than 400 records from 9 intermediate-depth earthquakes with moment magnitudes M-w >5.0 was assembled and compiled for the BIGSEES national research project. These strong ground motions are used to compute the values of the soil amplification factor which is a key parameter in the definition of the elastic response spectrum defined in Eurocode 8 (EN 1998-1). The strong ground motions are divided both in accordance with the soil category of the recording stations and with the control period To as well. The study of the acceleration response spectra as a function of magnitude, soil class and control period allows for the quantification of the amplification factors. Finally, the results obtained are compared with the design values from Eurocode 8 (EN 1998-1). This study comes at a time when Romania is harmonizing the national codes with the European design codes.

Authors:
Pavel F., Văcăreanu R., Ionescu C., Iancovici M., Sercaianu M.

Abstract:
This study focuses on the investigation of spectral characteristics of ground motions recorded from intermediate-depth Vrancea earthquakes using Newmark-Hall-type response spectrum. The database consists of more than 700 horizontal components recorded during 10 Vrancea earthquakes. In the first step of the analysis, the component-to-component variability is assessed and the corresponding influence of various parameters (earthquake magnitude, peak ground acceleration, soil class, position of the seismic station, or instrument type) is evaluated. Subsequently, the correlation between the spectral acceleration and the values of the peak ground motion parameters (acceleration, velocity, and displacement) is investigated. The analyses reveal an important influence of the magnitude and a significant influence of the soil class (in the case of large magnitude earthquakes) on the results. These findings are validated through the use of the analysis of variance (ANOVA) method. The computed response amplification factors for the Newmark-Hall type spectrum are similar with those from other studies in the literature. Finally, a check of three control periods such as T-B, T-E, and T-F of the Newmark-Hall-type spectrum yields results somewhat different from the ones given in the Romanian seismic design code P100-1 or in Eurocode 8.

Authors:
Pavel F., Văcăreanu R., Ionescu C., Iancovici M., Sercaianu M.

Abstract:
A systematic investigation of the applicability of several ground motion prediction models for Vrancea intermediate-depth seismic source is conducted in this research. Two ground motion prediction models recommended by previous evaluations (Vacareanu et al. in Bull Earthq Eng 11(6): 1867-1884, 2013a; Pavel et al. in Earthq Struct 6(1): 1-18, 2014), as well as two new state-of-the-art ground motion prediction equations (Vacareanu et al. in J Earthq Eng, 2013b; Earthq Struct 6(2): 141-161, 2014) are tested using an increased strong ground motion database consisting of 150 recordings from Vrancea subcrustal earthquakes. The evaluation is performed by using several goodness-of-fit parameters from the literature. Moreover, the applicability of the single-station sigma method is also investigated by using the same strong ground motion database recorded in 30 seismic stations from southern and eastern Romania. The influence of the soil conditions on the numerical results obtained in this study is investigated and discussed using the results provided by the analysis of variance method. The impact of the single-station standard deviation on the levels of seismic hazard is also assessed in this study, and the results show, in the analyzed cases, significant reductions in the hazard levels.

Authors:
Ioane D., Diaconescu M., Chitea F., Garbacea G.

Abstract:
In urban planning activities, besides a detailed seismic zonation, knowledge of the areal distribution of active faults, and particularly of faults crossing the city in heavily built districts, may be valuable in numerous cases. This chapter aims to identify active faults or fractures in Bucharest, a large city developed over thick layers of Quaternary unconsolidated sediments. To achieve this goal, the research is based on an integrated analysis of all existing relevant data coming from geology, geomorphology, geophysics and seismology. Another purpose is to understand the role of faults in the spatial variability of seismic damaging effects on buildings in view of a better future urban planning. The N-S fault system seems to be involved in neotectonics, affecting the geomorphology between Bucharest and Ploiesti cities. It could represent an active transcrustal fault, the deepest seismic event recorded within Bucharest at subcrustal depth being located on its southern prolongation. Within Bucharest the presence of faults affecting Pleistocene sediments was previously illustrated using borehole data, shallower vertical displacements of Quaternary formations along faults being interpreted in this study. The existing seismic reflection data recorded within Bucharest was used to interpret shallow faults considered as active or capable faults crossing Quaternary sedimentary deposits.

Authors:
Armas I., Radulian M.

Abstract:
The current paper is a piece of exploratory research, having as its purpose the evaluation of seismic risk spatial patterns for Bucharest, the capital of Romania. In this paper, risk (expressed in terms of risk indices) is calculated as a combination of hazard and vulnerability information, based on the semi-quantitative technique of multi-criteria spatial analysis. The scale of analysis was considered at the level of the census units (2002). The hazard component consists of the probability of occurrence of two scenarios: (1) an occurred earthquake that is a typical hazard case for the Vrancea region (event of 30 August 1986, M-w = 7.1) and (2) a computed seismic hazard for the largest magnitude earthquake expected to be generated in Vrancea (M-w = 7.7). In both cases, the seismic hazard is expressed in terms of peak ground acceleration (PGA) values. The total vulnerability index is obtained using four groups of indicators: natural environment, physical, social and economical indicators. The overall vulnerability to seismic hazard is assessed by comparing total vulnerability with the compound capacity factor. The resulting risk indices are relative, expressed by numerical values, ranging between 0 and 1, that do not have a direct meaning of expected losses. The spatial pattern of risk shows a significant increase in the case of the maximum expected event as compared with the 1986 earthquake case, particularly in the central part of the city. As a general conclusion, only the strongest earthquakes are really dangerous for Bucharest.

Authors:
Radulian M., Popescu E., Borleanu F., Diaconescu M.

Abstract:
The seismicity at the contact between the Getic Depression and the South Carpathians is part of the overall seismicity characterizing the contact of the Moesian Platform and the South Carpathians orogen. The December 2011-January 2012 earthquake sequence that occurred close to Tg-Jiu city provides the best data set for the seismic activity in the region. The seismic source parameters are estimated for 15 events of the sequence using the empirical Green's function and spectral ratio techniques. We selected 3 main events and 12 associated collocated small events as empirical Green's functions to calculate the spectral ratios and determine the relative source time functions. Estimates of the source duration and corner frequency imply stress drop values in the range of 6-112 MPa. Relative small radius of the source and high stress drops suggest an intraplate type behaviour. The scaling relationships investigated comply well with similar relationships in other regions in the world and in other seismogenic areas in the South Carpathians region.

Authors:
Bala A.

Abstract:
Bucharest, the capital city of Romania, with more than 2 million inhabitants, is considered as a natural disaster hotspot by a recent global study of the World Bank and the Columbia University (Dilley M et al. Natural disaster hotspots: a global risk analysis. International Bank for Reconstruction and Development/The World Bank and Columbia University, Washington, DC in 2005). Therefore, it is classified as the second metropolis in Europe, after Istanbul, subjected to important losses in the case of a destructive Vrancea earthquake with moment magnitude greater than seven. Four major earthquakes with moment magnitudes between 6.9 and 7.7 hit Bucharest in the last 68 years. The most recent destructive earthquake on March 4, 1977, with a moment magnitude of 7.4, caused about 1,500 casualties in the capital alone. All disastrous intermediate-depth earthquakes are generated within a small epicentral area-the Vrancea seismogenic region-about 150 km northeast of Bucharest. Thick unconsolidated sedimentary layers below Bucharest amplify the arriving seismic waves causing severe destruction. Ten 50-m-deep boreholes are drilled in the metropolitan area of Bucharest in order to obtain a unique, homogeneous dataset of seismic, soil-mechanic and elasto-dynamic parameters. Cores for dynamic tests were extracted, and vertical seismic profiles were performed to obtain an updated site amplification model related to earthquakes waves. The boreholes are placed near former or existing seismic station sites to allow a direct comparison and calibration of the borehole data with previous seismological measurements. A database containing geological characteristics for each sedimentary layer, geotechnical parameters measured on rock samples, P- and S wave velocity and density for each sedimentary layer is set up, as a result of previous papers with this subject. Direct data obtained by the geophysical methods in the new boreholes drilled in Bucharest City, as well as from laboratory measurements, are used as input data in the program SHAKE2000. Results are obtained in the form of spectral acceleration response, and peak acceleration in depth is computed for every site in which in situ measurements were performed. The acceleration response spectra correspond to the shear-wave amplifications due to the models of sedimentary layers down to (a) 50 m depth; (b) 70 m depth; and (c) 100 m depth. A comparison of the acceleration response spectra obtained by modelling at surface with a real signal recorded at surface is obtained in three sites, as test sites for the three depths considered, in order to calibrate the results obtained by equivalent linear method of the seismic site response.

Authors:
Rogozea M., Marmureanu G., Radulian M., Toma D.

Abstract:
The aim of this paper is to analyze the great event that occurred on January 23, 1838 (magnitude A(w) = 7.5 in the Romanian catalogue). Valuable information has been collected from original or compiled historical sources, such as chronicles and manuscripts on that time, and related books and reports. The historical data are critically analyzed and, on the basis of our investigation, we showed the degree of significance of the earthquake parameters, as resulted from the effect distribution. The pattern of the intensity data points as reevaluated for this historical earthquake is compared with the pattern of instrumentally recorded major earthquake of March 4, 1977, the two events assumed to be similar as hypocenter location, source parameters and rupture propagation.

Authors:
Bala A., Hannich D., Ehret D., Huber G.

Abstract:
Bucharest, the capital of Romania with about 2.5 million inhabitants, is frequently struck by intense, damaging earthquakes (in recent years in 1940, 1977, 1986 and 1990). In 1995 a Collaborative Research Center 461 (CRC-461) entitled: "Strong Earthquakes - a Challenge of Geosciences and Civil Engineering" was established in July 1996 and ended in December 2007. It was funded by the German Research Foundation and supported by the State of Baden-Wurttenmberg, as well as the University of Karlsruhe (TH), actually Karlsruhe Institute of Technology (KIT). The CRC aimed strategic research in the field of strong earthquakes with regional focus on the Vrancea seismic events in Romania. Between 1995-2007 several research works were done in Romania, with the support of several Romanian research institutes and the University of Bucharest. One of the research questions was, if liquefaction can occur during strong earthquakes within the shallow sandy layers in Bucharest. As known, strong earthquakes can cause, under certain geologic conditions, liquefaction and therewith ground failure as sand boils, lateral spreading, or differentiated subsidence. Thus in 2005 a research work begun to analyze the liquefaction risk for Bucharest. For this purpose, at 10 representative sites in Bucharest, Seismic Cone Penetration Tests (SCPTu) were executed. An area-wide evaluation of the liquefaction probability in Bucharest was established. The "factor of safety" (Fs) against liquefaction and the "probability of liquefaction" (PL) were computed from the obtained test-data. For the first time, maps of the "liquefaction potential index" (Li) and of the "liquefaction severity index" (Ls) for Bucharest were outlined. These maps show how severe liquefaction phenomena can occur during strong Vrancea earthquakes in Bucharest.

Authors:
Toma-Dănila D.

Abstract:
Considering the various effects of natural disasters, and the need for a fast intervention and recovery time, before facing the associated problems it is needed to mitigate the risks. A basic and initial step is to assess the vulnerability in high risk areas. The importance of a transport network is major, whether it is a road, railway (for access) or pipe (for resources) network. Various methods were described for analyzing their behavior to disastrous events (like earthquakes, landslides, flooding). The methodology proposed in this study integrates all related input data within a GIS software, adding by so the spatial dimension, and adapt the cost-distance method to obtain fictive costs that translate into vulnerability states for each point of a network. Also, the hot-points that can determine detour costs are taken into consideration, by means of random "What if?'' scenarios that are generated by an automation model. The fact that the cost-distance method requires origins to which the costs will refer it is important, because the vulnerability values will also be related to how hard it is for an emergency intervention team to reach a certain segment of the network. Because of the various degrees of freedom in the methodology, different methods can be also added to the actual core, in order to serve the purpose, whether it is emergency route analysis, road planning or loss estimation assessment. In order to test and exemplify the methodology and the results, a road network seismic vulnerability assessment example is presented, for a Romanian County right on top of the Vrancea Seismic Area. Specific details are given about the possibilities to implement the methodology.

Authors:
Moldovan I.A., Apostol B.F., Moldovan A., Ionescu C., Placinta A.O.

Abstract:
The Vrancea seismically active region of Romania, situated far-from active plate boundaries, can be characterized by small-large intermediate-depth earthquakes and small-moderate normal ones. The intermediate-depth earthquakes are destructive when larger than magnitude Mw 7.2. A bio-location methodology has been used trying to map crustal faults in Vrancea Depression and to indicate stress variations before and after intermediate-depth earthquakes. Bio-location data obtained across two perpendicular faults at Plostina, Vrancea, indicated a possible stress transfer from faults situated at intermediate-depth of 70-150 km, to faults situated in the Earth's crust at 0-40 km, before and after intermediate-depth earthquakes larger than local magnitude 3.0.

Authors:
Zaharia B., Tataru D., Grecu B., Ionescu C., Tibu S., Bica-Brisan N., Georgescu E.S.

Abstract:
The seismic risk in Romania is one of the highest in Europe, and thus understanding the earthquake phenomena and their effects at the earth surface represents an important step toward the education of population in earthquake affected regions of the country and aims to raise the awareness about the earthquake risk and possible mitigation actions. In this direction, the introduction of the seismological education in schools was welcomed with great interest. The Romanian Educational Seismic Network is a national project with many educational, scientific and social goals and represents an innovative program in Romania. The main educational objectives are referring to: training students and teachers in the analysis and interpretation of seismological data, preparing educational materials, designing and testing didactic activities. The scientific objective is to introduce in schools the use of scientific instruments like seismographs (SEP Seismometer) and experimental methods (seismic data analysis) that are usually restricted to research laboratories. The main product is to create an earthquake database which will be used by students and teachers for educational purposes. Regarding the social objectives, the project represents an effective instrument for informing and raising seismic risk awareness. The network consist of nine seismic stations with SEP seismometers installed in high-schools from the most important seismic areas (Vrancea, Banat, Fagaras, Dobrogea), vulnerable cities (Bucharest, Iasi) or high populated places (Cluj, Sibiu, Timisoara, Zalau). The educational materials consist of a collection entitled "Earthquakes and their effects", which includes educational materials for all pre-university education classes taking the form of two books (except preschool level), one for teachers and one for students. They are governed by the concept "learning by doing". Applying this concept the students will develop scientific aptitudes (measurements, direct observations, theory formulation and verification, database study) and they will be attracted to domain as Geology, Geography, Physics, Mathematics, Informatics, etc. Teaching modules include laboratory exercises like earthquake location and magnitude estimation using waveforms recorded by their school seismometers, and valuables information on how the earthquake affects the surrounding environment and buildings.

Authors:
Ren Y., Grecu B., Stuart G., Houseman G., Hegedus E.

Abstract:
We use ambient noise tomography to investigate the crust and uppermost mantle structure beneath the Carpathian-Pannonian region of Central Europe. Over 7500 Rayleigh wave empirical Green's functions are derived from interstation cross-correlations of vertical component ambient seismic noise recordings (2005-2011) using a temporary network of 54 stations deployed during the South Carpathian Project (2009-2011), 56 temporary stations deployed in the Carpathian Basins Project (2005-2007) and 100 permanent and regional broad-band stations. Rayleigh wave group velocity dispersion curves (4-40 s) are determined using the multiple-filter analysis technique. Group velocity maps are computed on a grid of 0.2 degrees x 0.2 degrees from a non-linear 2-D tomographic inversion using the subspace method. We then inverted the group velocity maps for the 3-D shear wave velocity structure of the crust and uppermost mantle beneath the region. Our shear wave velocity model provides a uniquely complete and relatively high-resolution view of the crustal structure in the Carpathian-Pannonian region, which in general is validated by comparison with previous studies using other methods to probe the crustal structure. At shallow depths (< 10 km) we find relatively high velocities below where basement is exposed (e.g. Bohemian Massif, Eastern Alps, most of Carpathians, Apuseni Mountains and Trans-Danubian Ranges) whereas sedimentary areas (e.g. Vienna, Pannonian, Transylvanian and Focsani Basins) are associated with low velocities of well defined depth extent. The mid to lower crust (16-34 km) below the Mid-Hungarian Line is associated with a broad NE-SW trending relatively fast anomaly, flanked to the NW by an elongated low-velocity region beneath the Trans-Danubian Ranges. In the lowermost crust and uppermost mantle (between 30 and 40 km), relatively low velocities are observed beneath the Bohemian Massif and Eastern Alps but the most striking features are the broad low velocity regions beneath the Apuseni Mountains and most of the Carpathian chain, which likely is explained by relatively thick crust. Finally, most of the Pannonian and Vienna Basin regions at depths > 30 km are relatively fast, presumably related to shallowing of the Moho consequent on the extensional history of the Pannonian region.

Authors:
Stanciu A.C., Russo R.M., Mocanu V.I., Munteanu L.

Abstract:
We present new splitting measurements for SKS and SKKS phases recorded at four broadband seismic stations located within the Carpathian Arc, in the eastern part of the Transylvanian Basin. We made 75 measurements, of which 58 are nulls and 17 show clear splitting. We used two methods to estimate splitting parameters, phi (the fast polarization direction) and delta t (the delay time between fast and slow split shear waves): minimization of energy on the horizontal component corresponding to the minimum eigenvalue of the polarization matrix, and simultaneous linearization of split waves from a suite of earthquakes recorded at a given station. We consistently observed no splitting at station IACB, in the northern part of the study area, for a range of well-recorded earthquakes at different backazimuths; we consider the station splitting to be null. Null splitting here is consistent with several possible tectonic scenarios, including downwelling of asthenospheric material as a result of the sinking Vrancea body, asthenospheric upwelling beneath Ciomadul volcano, or lack of anisotropic fabric development in the large Ciomadul magma chamber beneath the station. Fast polarized shear waves trend NW-SE at CHDM, in the Transylvanian Basin, and at PMAR, which lies at the boundary between the Transylvanian Basin and the E-W-striking Southern Carpathians; these fast directions are consistent with a regional trend in splitting phi azimuths over much of the Eastern Carpathians, the East European and Moesian Platforms, and the northwestern Transylvanian Basin away from the Vrancea Bend Zone. The regional NW-SE splitting trend parallels the NW-to-SE temporal migration of Neogene volcanism along the Eastern Carpathians, and is likely due to a combination of southeastward rollback of the Vrancea high velocity body and simultaneous southwestwards absolute plate motion of the thick leading edge of the East European Platform (Tornquist-Teisseyre Suture Zone), which together constrain regional mantle flow. Fast shear wave polarization, phi, at station COMD, at the juncture between the Vrancea Bend Zone and the Transylvanian Basin, trends NE-SW, consistent with splitting at stations VOIR and MLR in the Southern Carpathians. Splitting at these stations reflects perturbed mantle flow in the vicinity of the Vrancea body, which entails an abrupt change from NE-SW at VOIR to NNW-SSE at PMAR, consistent with redirection of mantle flow along the northwestern side of the Vrancea body. Delay times at the three stations with clear splitting vary from 0.96 to 2.73 s, indicating either the presence of an anisotropic layer ranging between 100 km thick beneath CHDM and 300 km beneath PMAR, or an unusually strong anisotropic fabric beneath the latter. (C) 2013 Elsevier Ltd. All rights reserved.

Authors:
Ivan M., Wang R.J.

Abstract:
Amplitude ratio of 30 short-period conspicuous P5KP and PKPab phases from five intermediate depth or deep events in Fiji-Tonga recorded at European stations around 150A degrees distance shows a mean value two to three times the ratio of the synthetic amplitudes obtained by the normal-mode theory (and ak135 model) or by full-wave theory (and PREM). There is a large variance in the results, also observed in five amplitude ratios from one event in Argentina observed at temporary stations in China around 156A degrees. Global recordings of three major deep earthquakes in Fiji, Bonin, and Western Brazil observed at ASAR, WRA, and ZRNK arrays, at 59 North America stations and at six South Pole stations displayed conspicuous P4KP and PcP (or ScP) phases. The amplitude ratio values of P4KP vs P(S)cP are sometimes almost one order of magnitude larger than the corresponding values of the synthetics. In both cases, arrival times and slowness values (corrected for ellipticity and station elevation) at the distances up to 23A degrees beyond the A cutoff point predicted by ray theory match both the synthetics, suggesting the observations are the AB branch of PmKP (m = 4, 5) around 1 Hz. In disagreement to ray theory, no reliable BC branch is observed neither on the recordings nor on the normal-mode synthetics. The high amplitude ratio values cannot be explained by realistic perturbations of the velocity or attenuation values of the global models in the proximity of the core-to-mantle boundary (CMB). We speculate that the focusing effects and/or strong scattering most likely associated to some anomalous velocity areas of the lowermost mantle are responsible for that. The results suggest limitations of the previous evaluations of the short-period attenuation in the outer core from PmKP amplitudes (m a parts per thousand yenaEuro parts per thousand 3), irrespective of the fact that they are obtained by using ray theory, normal-mode or full-wave synthetics. Attempts to use PmKP arrival times in order to refine velocity structure in the proximity of CMB should be also regarded with care if the propagation times have been computed with ray theory.

Authors:
Panaiotu C.G., Jicha B.R., Singer B.S., Tugui A., Seghedi I., Panaiotu A.G., Necula C.

Abstract:
Quaternary volcanism in the Persani Mountains forms an Na-alkali basaltic province inside the bend area of the Carpathians in the southeastern part of Europe. Previous K-Ar ages and paleomagnetic data reveal several transitional virtual geomagnetic poles, which were tentatively associated with the Cobb Mountain subchron and a Brunhes chron excursion. We report a new paleomagnetic and rock-magnetic study coupled with Ar-40/Ar-39 geochronology to better constrain the age of geomagnetic reversals or excursions that might be recorded and the timing of volcanism. Of the paleomagnetic directions obtained from sampled lava flows 4 are reversed polarity, 19 are normal polarity and 16 have transitional polarity. Ar-40/Ar-39 plateau ages determined from incremental heating experiments on groundmass indicate that two of the reversely magnetized lavas erupted at 1142 +/- 41 and 800 +/- 25 ka, four of the normally magnetized lavas erupted at 1060 +/- 10, 1062 +/- 24, 684 +/- 21, and 683 +/- 28 ka, and two transitionally magnetized lavas formed at 1221 +/- 11 and 799 +/- 21 ka. Both the new Ar-40/Ar-39 ages and the paleomagnetic data suggest at least five episodes of volcanic activity with the most active periods during the Jaramillo and Brunhes chrons. This results shows that the last phases of alkalic and calc-alkaline magmatism in the South-East Carpathians were contemporaneous. The age of the older transitionally magnetized lava flow is within error of recent unspiked K-Ar and astrochronologic ages for the reversal that defines the onset of the Cobb Mountain normal polarity subchron. The age of the younger transitional lava is similar to that of an excursion that preceded the Matuyama-Brunhes polarity reversal and which has come to be known as the Matuyama-Brunhes precursor. Omitting the excursion data, the dispersion of the virtual geomagnetic poles (around 19 degrees) is larger than the expected value around 45 degrees N from the global compilation, but closer to the value obtained only from the Time Averaged geomagnetic Field Initiative studies. (C) 2013 Elsevier B.V. All rights reserved.

Authors:
Kronrod T., Radulian M., Panza G., Popa M., Paskaleva I., Radovanovich S., Gribovszki K., Sandu I., Pekevski V.

Abstract:
A unique macroseismic data set for the strongest earthquakes occurring since 1940 in the Vrancea region is constructed by a thorough review of all available sources. Inconsistencies and errors in the reported data and in their use are also analysed. The final data set, which is free from inconsistencies, including those at the political borders, contains 9822 observations for the strong intermediate-depth earthquakes: 1940, M-w = 7.7; 1977, M-w = 7.4; 1986, M-w = 7.1; 1990, May 30, M-w = 6.9; 1990, May 31, M-w = 6.4; and 2004, M-w = 6.0. This data set is available electronically as Supplementary data to the present paper. From the discrete macroseismic data, the continuous macroseismic field is generated using the methodology developed by Molchan et al. (2002). The procedure, along with the unconventional (smoothing method) modified polynomial filtering (MPF), uses the diffuse boundary (DB) method, which visualises the uncertainty in the isoseismal boundaries. The comparison of DBs with previous isoseismal maps supplies a good evaluation criterion of the reliability of earlier published maps. The produced isoseismals can be used not only for the formal comparison of the observed and theoretical isoseismals but also for the retrieval of source properties and the assessment of local responses (Molchan et al., 2011). (c) 2013 Elsevier B.V. All rights reserved.

Authors:
Mărmureanu G., Mărmureanu A., Cioflan C.O., Ionescu C.

Abstract:
In a world of uncertainty, the only constant is change and rapid change produces a multitude of diverse facts. Risk is an integral part of life. While no country in the world is entirely safe, the lack of capacity to limit the impact of hazards remains a major burden for all countries and while the world has witnessed an exponential increase in human and material losses due to natural disasters, there is a need to reverse trends in vulnerability to earthquakes. Available data prove that natural disasters from earthquakes can cause considerable damages, with potentially severe effects to urban environment. Earthquakes cascade as chaotic chain reactions through the natural and built environments; therefore, seismic hazard and risk are time-dependent quantities. On the other hand, environmental degradation increases the intensity of natural disasters, and is often the factor that transforms natural hazards, into a disaster. In World, earthquakes are responsible for 15% of total number of events, and 30% of the total damages (Freeman, 2000). Last strong Vrancea earthquake on March 4, 1977 (Mw=7.4, h=95 km): 1578 dead and 11,321 injured, 36 ruined/destroyed blocks in Bucharest, 32,900 houses collapsed or severely damaged; 35,000 families homeless, tens of thousands (64,000) of buildings damaged from Iasi and Bacau to Craiova, many other damages and destructions in the industry and economy; the downtown of Bacau was completely damaged etc. The goal of the paper is to enhance our capability to decrease the effects of strong and deep Vrancea earthquakes on urban and built environment, especially in Moldavian area. The practical goal is to enable new geo-technologies for reducing risk and improving community resilience. Specific fundamental and applied researches were developed last years by National Institute for Earth Physics sustained by national legislation and regulations as well as European Programs: FP-7, Cross-Border etc. The priority of protecting the environment is emphasized. This knowledge can be very fruitfully used by civil engineers in the design of new seismic resistant constructions and in the reinforcement of the existing built environment, and, therefore, supply a particularly powerful tool for the prevention aspects of Civil Defense.

Authors:
Oros E.

Abstract:
We analyze the seismic activity recorded between January and March 2012 near the city of Timisoara. We identified two earthquake sequences during this time interval: one started on 07.01.2012 at a few kilometers SW of the city (N = 3 events, Depic = 1-7 km, Mwmin = 2.1, Mwmax = 3.1, hmin = 7.1 +/- 1.6 kin, hmax = 9.8 +/- 1.0 km), the other with the main event on 09.01.2012 located at 30 km East of the city (N = 20 events, Mwmin = 0.4, Mwmax = 3.4, hmin = 2 +/- 2.6 km, hmax = 14.5 +/- 1.7 km). Epicentral zones of these sequences have elongated shapes and develop along a major fault system of the region, particularly at its intersection with other deeply fractured structures. The depth distribution displays three small groups of earthquakes at 2-5 km, 5-11 km and 11-16 km, respectively. Focal mechanism solutions estimated for the main events of the sequence show possible causative faults EW to ENE-WSW oriented, consistent with seismicity, geology, local stress field and seismotectonics.

Authors:
Bala A.

Abstract:
Ten 50 m deep boreholes are drilled in the metropolitan area of Bucharest in order to obtain a unique, homogeneous dataset of seismic, soil-mechanic and elasto-dynamic parameters. Cores for dynamic tests were extracted and vertical seismic profiles were performed to obtain an updated site amplification model related to earthquakes waves. The boreholes are placed near former or existing seismic station sites to allow a direct comparison and calibration of the borehole data with previous seismological measurements. A database containing geological characteristics for each sedimentary layer, geotechnical parameters measured on rock samples, P- and S-wave velocity, density for each sedimentary layer is set up. Results obtained by the down-hole method in the new boreholes drilled in Bucharest City as well as from laboratory measurements are used as input data in the program SHAKE2000. Spectral acceleration response and peak acceleration in depth are computed for every site in which in situ measurements were performed. The acceleration response spectra correspond to the shear-wave amplifications due to the models of sedimentary layers down to: a) 50 m depth; b) 70 m depth; c) 100 m depth. A comparison with a real signal recorded at surface is made in order to calibrate the models used in the equivalent-liniar evaluation of the seismic site response.

Authors:
Constantin A.P., Pantea A.

Abstract:
On October 27, 2004, a moderate size earthquake occurred in the Vrancea seismogenic region (Romania). The Vrancea seismic zone is an area of concentrated seismicity at intermediate depths beneath the bending area of the southeastern Carpathians. The 2004 M (w) = 6 Vrancea subcrustal earthquake is the largest seismic event recorded in Romania since the 1990 earthquakes. With a maximum macroseismic intensity of VII Medvedev-Sponheuer-Karnik (MSK-64) scale, the seismic event was felt to a distance of 600 km from the epicentre. This earthquake caused no serious damage and human injuries. The main purpose of this paper is to present the macroseismic map of the earthquake based on the MSK-64 intensity scale. After the evaluation of the macroseismic effects of this earthquake, an intensity dataset has been obtained for 475 sites in the Romanian territory. Also, the maximum horizontal accelerations recorded in the area by the K2 network are compared to the intensity values.

Authors:
Apostol B.F.

Abstract:
We examine the elastic waves excited on the plane surface of an isotropic body (half-space) by an oscillatory force which decreases exponentially with the distance from the surface. We define the "H/V"-ratio as the ratio of the intensity of the waves with polarization parallel to the surface (horizontal waves) to the intensity of the waves with polarization perpendicular to the surface (vertical waves). It is shown that this ratio may exhibit a maximum value or a resonance. Under reasonable assumptions, the resonance frequency may be close to the frequency of the in-plane transverse (shear) waves. It may serve to determine the Poison ratio, or to characterize the sub-surface structure of the body. The resonance is particularly apparent for a vertical force.

Authors:
Pantea A., Constantin A.P.

Abstract:
In this paper, the macroseismic effects of the subcrustal earthquake in Vrancea (Romania) that occurred on March 4, 1977, have been re-evaluated. This was the second strongest seismic event that occurred in this area during the twentieth century, following the event that happened on November 10, 1940. It is thus of importance for our understanding of the seismicity of the Vrancea zone. The earthquake was felt over a large area, which included the territories of the neighboring states, and it produced major damage. Due to its effects, macroseismic studies were developed by Romanian researchers soon after its occurrence, with foreign scientists also involved, such as Medvedev, the founder of the Medvedev-Sponheuer-Karnik (MSK) seismic intensity scale. The original macroseismic questionnaires were re-examined, to take into account the recommendations for intensity assessments according to the MSK-64 macroseismic scale used in Romania. After the re-evaluation of the macroseismic field of this earthquake, the intensity dataset was obtained for 1,620 sites in Romanian territory. The re-evaluation was necessary as it has confirmed that the previous macroseismic map was underestimated. On this new map, only the intensity data points are plotted, without tracing the isoseismals.

Authors:
Apostol B.F.

Abstract:
The classical theory of scattering of longitudinal waves (sound) by small inhomogeneities (scatterers) in an ideal fluid is generalized to a distribution of scatterers and such as to include the effect of the inhomogeneities on the elastic properties of the fluid. The results are obtained by a new method of solving the wave equation with spatial restrictions (caused by the presence of the scatterers), which can also be applied to other types of inhomogeneities (like surface roughness, for instance). A coherent forward scattering is identified for a uniform distribution of scatterers (practically equivalent with a mean-field approach), which is due to the fact that our treatment does not include multiple scattering. The reflected wave is obtained for a half-space (semi-infinite fluid) of uniformly distributed scatterers, as well as the field diffracted by a perfect lattice of scatterers. The same method is applied to a (inhomogeneous) rough surface of a semi-infinite ideal fluid. A perturbation-theoretical scheme is devised, with the roughness function as a perturbation parameter, for computing the waves scattered by the surface roughness. The waves scattered by the rough surface are both waves localized (and propagating only) on the surface (two-dimensional waves) and waves reflected back in the fluid. They exhibit directional effects, slowness, attenuation or resonance phenomena, depending on the spatial characteristics of the roughness function. The reflection coefficients and the energy carried on by these waves are calculated both for fixed and free surfaces. In some cases, the surface roughness may generate waves confined to the surface (damped, rough-surface waves).

Authors:
M. Stucchi, A. Rovida, A. A. Gomez Capera, P. Alexandre, T. Camelbeeck, M. B. Demircioglu, P. Gasperini, V. Kouskouna, R. M. W. Musson, M. Radulian, K. Sesetyan, S. Vilanova, D. Baumont, H. Bungum, D. Fäh, W. Lenhardt, K. Makropoulos, J. M. Martinez Solares, O. Scotti, M. Živčić, P. Albini, J. Batllo, C. Papaioannou, R. Tatevossian, M. Locati, C. Meletti, D. Viganò & D. Giardini

Abstract:
In the frame of the European Commission project "Seismic Hazard Harmonization in Europe" (SHARE), aiming at harmonizing seismic hazard at a European scale, the compilation of a homogeneous, European parametric earthquake catalogue was planned. The goal was to be achieved by considering the most updated historical dataset and assessing homogenous magnitudes, with support from several institutions. This paper describes the SHARE European Earthquake Catalogue (SHEEC), which covers the time window 1000-1899. It strongly relies on the experience of the European Commission project "Network of Research Infrastructures for European Seismology" (NERIES), a module of which was dedicated to create the European "Archive of Historical Earthquake Data" (AHEAD) and to establish methodologies to homogenously derive earthquake parameters from macroseismic data. AHEAD has supplied the final earthquake list, obtained after sorting duplications out and eliminating many fake events; in addition, it supplied the most updated historical dataset. Macroseismic data points (MDPs) provided by AHEAD have been processed with updated, repeatable procedures, regionally calibrated against a set of recent, instrumental earthquakes, to obtain earthquake parameters. From the same data, a set of epicentral intensity-to-magnitude relations has been derived, with the aim of providing another set of homogeneous Mw estimates. Then, a strategy focussed on maximizing the homogeneity of the final epicentral location and Mw, has been adopted. Special care has been devoted also to supply location and Mw uncertainty. The paper focuses on the procedure adopted for the compilation of SHEEC and briefly comments on the achieved results.

Authors:
Moldovan I.A.,Constantin A.P,Popescu E.,Placinta A.O.

Abstract:
The main goal of this paper is rating the dams from the South-Western part ofRomania (Danube, Olt, Jiu and Lotru rivers) into seismic risk classes. Dam owners andregulators must ensure that dams are safely operated and present no risk to the public in caseof an earthquake. While most old or new dams in recognized seismic regions have beenevaluated and analyzed for seismic loads, dams located in areas of moderate or infrequentseismicity have been given less systematic attention. In such cases, owners of many dams orofficials in charge of dam safety programs may consider comparative assessment of theseismic risk associated with their dams and establish priorities, as needed. Risk classes can beused to establish the necessity of detailed assessment of seismic safety of the dams and toestablish the priorities of these evaluations.The methodology which is used in this paper offers an easy way to evaluate the mostvulnerable hydrotechnical facilities among the multitude of dams in the Western part ofRomania that are affected by crustal-depth earthquakes from Banat and Danubian regions andby Vrancea intermediate depth earthquakes. The risk is expressed as a product between hazardand vulnerability. In particular, seismic risk in the case of hydrotechnical arrangements iscomputed as a product between seismic hazard (corresponding to the location of the respectivehydrotechnical arrangement) and the seismic vulnerability of the respective arrangement.Various risk factors and weighting points can be used to approximately quantify the Total RiskFactor (TRF) of any dam. The TRF depends on the dam type, age, size, the downstream riskpotential, and the dam vulnerability, which depends on the seismic hazard of the site. The damstructure influence is represented by the sum of capacity, height, and age risk factors. Thedownstream hazard factor is based on population and property at risk. The vulnerability ratingis a function of the site-dependent seismic hazard and observed performance of similar dams,as defined by a predicted damage factor.This procedure can be used to quickly asses S the potentially most vulnerable facilities in alarge dam inventory. The risk classification based on the TRF, provides guidance to damsafety officials to select appropriate evaluation procedure and to assign priorities for seismicsafety evaluation of the most critical dams.Key words: seismic hazard, risk classes, dams.

Authors:
Moldovan I.A.,Placinta A.O.,Constantin A.P.,Moldovan A.S.,Ionescu C.

Abstract:
The study presents a statistical cross-correlation between geomagneticanomalies, earthquake occurrence and solar magnetic storms. The workingdata are from: (i) geomagnetic field records from Muntele Rosu (MLR)Observatory, and from Surlari (SUA) and/or Tihany (THY)INTERMAGNET Observatories; (ii) seismic data for the Vrancea sourcezone; and (iii) daily geomagnetic indices from the NOAA/Space WeatherPrediction Center. All of the geomagnetic datasets were recorded from 1996to the present, at MLR, SUA or THY, and they were automaticallycorrected using a LabVIEW program developed especially for this purpose,highlighting the missing or bad data. Missing data blocks were completedwith the last good measured value. After correction of the data, there werea number of issues seen regarding previous interpretations of thegeomagnetic anomalies. Some geomagnetic anomalies identified asprecursory signals were found to be induced either by increased solaractivity or by malfunction of the data acquisition system, which producedinconsistent data, with numerous gaps. The MLR geomagnetic data arecompared with the data recorded at SUA/THY and correlated withseismicity and solar activity. These 15 years of investigations cover morethan a complete solar cycle, during which time the solar-terrestrialperturbations have fluctuated from very low to very high values, providingthe ideal medium to investigate the correlations between the geomagneticfield perturbations, the earthquakes and the solar activity. The largestintermediate depth earthquake produced in this interval had a momentmagnitude Mw 6.0 (2004) and provided the opportunity to investigatepossible connections between local geomagnetic field behavior and localintermediate seismicity.

Authors:
Grecu B.,Neagoe C.,Tataru D.

Abstract:
The noise level of the Romanian broadband stations operating since 2006 has been studied in orderto identify the variations in background seismic noise as a function of time of day, season, and particularconditions at the stations. Power spectral densities and their corresponding probability densityfunctions are used in this paper to characterize the background seismic noise. At high frequencies(> 1 Hz), seismic noise seems to have cultural origin, since significant variations (up to 55 dB)between daytime and nighttime noise levels are observed at almost all of the stations. However,this variability appears not to influence the detection capabilities of the Romanian Seismic Networkin case of intermediate-depth earthquakes and earthquakes with magnitude over 3.0. For smallermagnitude events (Mw < 3), we showed that the number of stations detecting an event decreasesduring daytime. We studied the seasonal variation of the seismic noise for primary and secondarymicroseisms (with emphasize for the latter) and we demonstrated that the noise levels are higher inwinter than in summer. We also observed a shift of the double-frequency peak from lower periods insummer to longer periods in winter. The polarization analysis indicated that the main sources of secondarymicroseisms for stations close to the Black Sea are coming from the Black Sea, while for theothers the main sources are found in the Mediterranean Sea and Atlantic Ocean. Finally, the analysisof the probability density functions for stations located in different geologic conditions has pointedout that the noise level is higher for stations sited on softer formations than those sited on hard rocks.

Authors:
Ardeleanu L.,Grecu B.,Raileanu V.

Abstract:
he goal of the study is to analyze the distributions of peak groundacceleration, velocity and displacement from 18 moderate size undercrustal earthquakes(Mw 4.0-5.0), which occurred in the Vrancea region during the period 2008–2010. Thepatterns of the investigated ground motion parameters keep the general featuresobserved for the strong Vrancea earthquakes – a rapid decrease of the ground shakingin SE-NW direction, and a prominent asymmetry of the isolines. The variability noticedamong the individual distributions appears as a result of the combined effects of thehypocenter location within the seismogenic zone (focal depth and epicenter position)and diversity of the focal mechanisms.

Authors:
Ivan M., Wang R.

Abstract:
Amplitude ratio of 30 short-period conspicuousP5KP and PKPab phases from five intermediatedepth or deep events in Fiji-Tonga recorded at Europeanstations around 150° distance shows a meanvalue two to three times the ratio of the syntheticamplitudes obtained by the normal-mode theory (andak135 model) or by full-wave theory (and PREM).There is a large variance in the results, also observedin five amplitude ratios from one event in Argentinaobserved at temporary stations in China around 156°.Global recordings of three major deep earthquakes inFiji, Bonin, and Western Brazil observed at ASAR,WRA, and ZRNK arrays, at 59 North America stationsand at six South Pole stations displayed conspicuousP4KP and PcP (or ScP) phases. The amplitude ratiovalues of P4KP vs P(S)cP are sometimes almost oneorder of magnitude larger than the corresponding valuesof the synthetics. In both cases, arrival times andslowness values (corrected for ellipticity and stationelevation) at the distances up to 23° beyond the Acutoff point predicted by ray theory match both thesynthetics, suggesting the observations are the ABbranch of PmKP (m04, 5) around 1 Hz. In disagreementto ray theory, no reliable BC branch is observedneither on the recordings nor on the normal-modesynthetics. The high amplitude ratio values cannot beexplained by realistic perturbations of the velocity orattenuation values of the global models in the proximityof the core-to-mantle boundary (CMB). We speculatethat the focusing effects and/or strong scatteringmost likely associated to some anomalous velocityareas of the lowermost mantle are responsible for that.The results suggest limitations of the previous evaluationsof the short-period attenuation in the outer corefrom PmKP amplitudes (m≥3), irrespective of the factthat they are obtained by using ray theory, normalmodeor full-wave synthetics. Attempts to use PmKParrival times in order to refine velocity structure in theproximity of CMB should be also regarded with care ifthe propagation times have been computed with raytheory.

Authors:
Toma-Danila D.

Abstract:
In the last years, thanks to the implementation of the ShakeMap software in real-time at the National Institute for Earth Physics(NIEP) and within the DACEA Project, a system that computes damage and loss estimates in (near) real-time for the Romanian-Bulgarian border region was installed at NIEP, producing data and maps for 7 Romanian Counties and 9 Bulgarian Districts.This paper presents both the integration mode and the results obtained by adding new counties into the implemented system, and also presents best ways for a GIS representation of the estimated damage. Of great interest is that the new counties – Vrancea and Bacau, are right on top of the active seismic area of Vrancea, compared to the previous analyzed counties that are more than 100km away from the epicentral area.There are many practical sides of the paper: based on past events it is illustrated how the damage might look like nowadays in avery exposed area and what are the risks to be dealt with, raising questions about new mitigating actions. Also, the certain accuracy of the loss assessment is validated, so that the new counties can be included in the real-time damage estimation system at NIEP.

Authors:
Moldovan I.A., Moldovan A., Biagi P.F., Placinta A.O.

Abstract:
The paper presents the Romanian VLF / LF monitoring system consisting in a radioreceiver – made by Elettronika S.R.L. (Italy) and provided by the Bari University – and theinfrastructure that is necessary to record and transmit the collected data. This system is a part of theinternational initiative INFREP. Through this initiative, originated in Italy, VLF / LF radio receiversare deployed in different locations in Europe. Each one is monitoring up to ten different transmissionsof radio stations across the continent. Information on electromagnetic fields’ intensities created bytransmitters at each receiving site and gathered from this network are indicating the quality of thepropagation along the paths between the receivers and transmitters. Studying the ionosphereinfluences on the electromagnetic waves’ propagation along a certain path is a method to put intoevidence possible modifications of ionosphere lower structure and composition as earthquakes’ precursor.The VLF / LF receiver installed in Romania was put into operation in February 2009 and hasproved its utility in the case of Abruzzo earthquake that occurred on 6th of April 2009 (Mw = 6.3).Since then, the receiver was relocated from Bucharest to the Black-Sea shore (Dobrogea SeismologicObservatory). Changing the receiving site produced unsatisfactory monitoring data, characterized bylarge fluctuations of the received signals’ intensities. Trying to understand this behavior has led to theconclusion that the electric component of the electromagnetic field was possibly influenced by thelocal atmospheric conditions (as aerosols’ concentrations could be). Starting from this observation wehave run some tests which have indicated that a loop-type antenna is more appropriate than a verticalantenna, especially for highly electric-field polluted environments. Very good results were obtainedwith this new configuration, even in the site located at the Black-Sea shore. Future improvements ofthe receiver analog front-end are still possible in order to get better monitoring data by rejecting theoff-band noise induced by the aerial high-voltage lines that are surrounding the site, so that for us toaccomplish the best achievable surveillance in VLF / LF bands, related to seismo-electromagneticphenomena.

Authors:
D'Alessandro A., Danet A., Grecu B.

Abstract:
Romania is an earthquake-prone area with a few-destructive earthquakes per century. The National Institute for Earth Physics carries out the seismic survey of Romania through the Romanian National Seismic Network (RNSN) consisting of 65 real-time seismic stations. Daily reports and monthly bulletins are delivered after routinely analyzing and processing the recorded data. In the present paper we applied the Seismic Network Evaluation through Simulation method for the RNSN configuration as it was in August 2011 to estimate the background noise level, assess the appropriateness of the velocity model adopted in routine location procedure, evaluate the hypocenter location uncertainty and determine the detection magnitude threshold. Areas of greater(southern Romania) and lower (Carpathians and Apuseni Mountains)background noise within the RNSN are identified by mapping the average power of noise in 1–12 Hz frequency range. The statistical study of the P and S phases residual times allow us to assess the appropriateness of the velocity model used in routine location. Both P- and S-wave velocity models can be optimized to improve the quality of the hypocenter location. As shown by our analysis, the RNSN is able to detect and locate earthquakes with ML magnitude above 2.5 anywhere on the Romanian territory, except the border areas, such as the Crisana–Maramures seismic source zone. Merging data from both sides of the border significantly improves the quality of hypocenter location in these areas.

Authors:
Molinari I., Raileanu V., Morelli A.

Abstract:
In the last two decades, south-central Europe and the Eastern Alps have been widely explored by many seismic refraction experiments (e.g., CELEBRATION 2000, ALP 2002, SUDETES 2003). Although quite detailed images are available along linear profiles, a comprehensive, three-dimensional crustal model of the region is still missing. This limitation makes this region a weak spot in continental-wide comprehensive representations of crustal structure. To improve on this situation, we select and collect 37 published active-source seismic lines in this region. After geo-referencing each line, we sample them along vertical profiles—every 50 km or less along the line—and derive P-wave velocities in a stack of homogeneous layers (separated by discontinuities: depth of crystalline basement, top of lower crust, and Moho). We finally merge the information using geostatistical methods, and infer S-wave velocity and density using empirical scaling relations. We present here the resulting crustal model for a region encompassing the Eastern Alps, Dinarides, Pannonian basin, Western Carpathians and Bohemian Massif, covering the region within 4551N and 1122E with a resolution of 0:2  0:2: We are also able to extend and update the map of Moho depth in a wider region within 3551N and 1245E; gathering Moho values from the collected seismic lines, other published dataset and using the European plate reference EPcrust as a background. All the digitized profiles and the resulting model are available online.

Authors:
Muco B., Alexiev G., Aliaj S., Elezi Z., Grecu B., Mandrescu N., Milutinovic Z., Radulian M., Ranguelov B., Shkupi D.

Abstract:
The assessment of geological hazard is a topic with significant interest for the Balkans. During the last decade of twentieth century, most of the countries in the region have embarked on the road of a hasty transitory period from totalitarian regimes to democracy. Development of free market economy has given rise to uncontrolled movement of people, fast construction of housing and facilities and unproportioned accumulation of population around and in big cities. Besides Greece, an old member of European Union, and two newcomers in the organization, Romania and Bulgaria, the other countries are all hoping to enter the Union as faster as they can. Many different candidate or fullfledged member country programs of European Community offer a lot of joint and crossborder projects for constructing road infrastructure and facilities. As development accelerates in the Balkans and given the intensive geohazard elements that this territory exhibits, it becomes increasingly important to understand, study, and map these elements for being aware of the damage to the total environment these hazards might cause. The geohazard map and assessment of some Balkan countries has been carried out through two scientific meetings in Ohrid, Macedonia, and Tirana, Albania during 2007. The map is compiled in the Albanian Geological Survey, Tirana, Albania in the scale 1:1,000,000. As a base map, we used the topographic map produced by VGI, formerly Yugoslavia mapping authorities. As a seismic layer in our map, we used the values of peak ground acceleration obtained from Global Seismic Hazard Assessment Program. Two catalogs were constructed: The first one that contains the crustal earthquakes (hypocentral depth within first 70 km) and the second one that contains intermediate earthquakes (hypocentral depth below 70 km). This work is largely based on previous studies and investigations by earth scientists and specialists of each country comprised in this territory. In this respect, the map we constructed should be considered as a preliminary composite geohazard map with the possibility to be enriched and added with other new elements and data in the future.

Authors:
Popescu E., Borleanu F., Rogozea M., Radulian M.

Abstract:
The goal of the paper is to investigate the most recent earthquake sequence (6–30 September 2008) generated in a characteristic seismicity cluster located in the crust, in the north-eastern part of the Vrancea intermediate-depth epicentral area (close to the Vrancioaia seismic station). Seismic source properties are determined using multiple approaches: empirical Green’s functions (EGF) deconvolution, spectral ratios technique and acceleration spectra analysis. For EGF and spectral ratios application, we associated to the main event (MD = 4.4) eight co-located aftershocks (2.0 ≤ MD ≤ 3.6), selected according to the requirements for empirical Green’s functions. The source parameters (seismic moment, corner frequency, rise time, source duration) are estimated as mean values for all the available pairs. In parallel, source parameters are retrieved from the analysis of the accelerometer spectra. The resulted source time functions are similar from one station to the other, suggesting negligible source directivity effects for the study events. The shape of the deconvolved source time function for the main shock of 6 September 2008 indicates a homogeneous rupture process in the focus with rupture duration of 0.24s. The multiple technique approach allows us to test the stability of the obtained parameters.

Authors:
Raileanu V., Tataru D., Grecu B.

Abstract:
A set of crustal data collected in the last decades across the Moesian platform are processed in order to derive a crustal model. The new crustal model comprises maps with depths to the top of the lower crust and Moho and thicknesses of the crystalline upper and lower crust. Some ranges of mean P-wave velocity in the upper and lower crust are assigned for the eastern and western sectors of the platform.

Authors:
Righetti F., Biagi P.F., Maggipinto T., Schiavulli L., Ligonzo T., Ermini A., Moldovan I.A., Moldovan A.S., Buyuksarac A., Silva H.G., Bezzeghoud M., Contadakis M. E., Arabelos D.N., Xenos T.D.

Abstract:
In 2008, a radio receiver that works in very low frequency (VLF; 20-60 kHz) and LF (150-300 kHz) bands was developed by an Italian factory. The receiver can monitor 10 frequencies distributed in these bands, with the measurement for each of them of the electric field intensity. Since 2009, to date, six of these radio receivers have been installed throughout Europe to establish a ‘European VLF/LF Network’. At present, two of these are into operation in Italy, and the remaining four are located in Greece, Turkey, Portugal, and Romania. For the present study, the LF radio data collected over about two years were analysed. At first, the day-time data and the night-time data were separated for each radio signal. Taking into account that the LF signals are characterized by ground-wave and sky-wave propagation modes, the day-time data are related to the ground wave and the night-time data to the sky wave. In this framework, the effects of solar activity and storm activity were defined in the different trends. Then, the earthquakes with M ≥5.0 that occurred over the same period were selected, as those located in a 300-km radius around each receiver/transmitter and within the 5th Fresnel zone related to each transmitter-receiver path. Where possible, the wavelet analysis was applied on the time series of the radio signal intensity, and some anomalies related to previous earthquakes were revealed. Except for some doubt in one case, success appears to have been obtained in all of the cases related to the 300 km circles for the ground waves and the sky waves. For the Fresnel cases, success in two cases and one failure were seen in analysing the sky waves. The failure occurred in August/September, and might be related to the disturbed conditions of the ionosphere in summer

Authors:
Rogozea M., Marmureanu Gh., Radulian M., Toma D.

Abstract:
The aim of this paper is to analyze the great event that occurred on January 23, 1838 (magnitude Mw = 7.5 in the Romanian catalogue). Valuable information has been collected from original or compiled historical sources, such as chronicles and manuscripts on that time, and related books and reports. The historical data are critically analyzed and, on the basis of our investigation, we showed the degree of significance of the earthquake parameters, as resulted from the effect distribution. The pattern of the intensity data points as reevaluated for this historical earthquake is compared with the pattern of instrumentally recorded major earthquake of March 4, 1977, the two events assumed to be similar as hypocenter location, source parameters and rupture propagation.

Authors:
Lang D.,Sergio Molina-Palacios S.,Lindholm C.,Balan S.F.

Abstract:
On March 4, 1977, an earthquake with amoment magnitude Mw 7.4 at a hypocentral depth of94 km hit the Vrancea region (Romania). In Bucharestalone, the earthquake caused severe damage to 33,000buildings while 1,424 people were killed. Under theumbrella of the SAFER project, the city of Bucharest,being one of the larger European cities at risk, waschosen as a test bed for the estimation of damage andconnected losses in case of a future large magnitudeearthquake in the Vrancea area. For the conduct ofthese purely deterministic damage and loss computations,the open-source software SELENA is applied.In order to represent a large event in the Vrancearegion, a set of deterministic scenarios were definedby combining ranges of focal parameters, i.e.,magnitude, focal depth, and epicentral location.Ground motion values are computed by considerationof different ground motion prediction equations thatare believed to represent earthquake attenuationeffects in the region. Variations in damage and lossestimates are investigated through considering differentsets of building vulnerability curves (provided byHAZUS-MH and various European authors) tocharacterize the damaging behavior of prevalentbuilding typologies in the city of Bucharest.

Authors:
Rogozea M., Radulian M., Marmureanu Gh., Mandrescu N., Paulescu D.

Abstract:
The purpose of this paper is to find historically-based arguments to validate or rectify the earthquake parameters as existing now in the catalogues. Systematic search for the original information collected from annals of time, reviews, notes on old religious writings, newspapers, etc. was carried out. In parallel, all the information available in the catalogues of earthquakes in the Carpathian region was considered. The historical data are critically analyzed and, on the basis of our investigation. Also, we tried to compensate for the uneven geographical distribution: clearly more systematic and rich documentation comes from Brasov (Transylvania) area as compared with other provinces, such as Wallachia and Moldova. Basically, only the events mentioned in at least two independent documentary sources were included in the revised catalogue. A significant fraction of the total catalogued events was proved to be improperly parameterized in the previous catalogues.

Authors:
Stucchi M., Rovida A., Gomez C.A.A., Alexandre P., Camelbeeck T., Demircioglu M.B., Kouskouna V., Gasperini P., Musson R.M.W., Radulian M., Sesetyan K., Vilanova S., Baumont D., Faeh D., Lenhardt W., Martinez S.J.M., Scotti O., Zivcic M., Albini P., Batllo J., Papaioannou C

Abstract:
In the frame of the European Commission project “Seismic Hazard Harmonization in Europe” (SHARE), aiming at harmonizing seismic hazard at a European scale, the compilation of a homogeneous, European parametric earthquake catalogue was planned. The goal was to be achieved by considering the most updated historical dataset and assessing homogenous magnitudes, with support from several institutions. This paper describes the SHARE European Earthquake Catalogue (SHEEC), which covers the time window 1000–1899. It strongly relies on the experience of the European Commission project “Network of Research Infrastructures for European Seismology” (NERIES), a module of which was dedicated to create the European “Archive of Historical Earthquake Data” (AHEAD) and to establish methodologies to homogenously derive earthquake parameters from macroseismic data. AHEAD has supplied the final earthquake list, obtained after sorting duplications out and eliminating many fake events; in addition, it supplied the most updated historical dataset. Macroseismic data points (MDPs) provided by AHEAD have been processed with updated, repeatable procedures, regionally calibrated against a set of recent, instrumental earthquakes, to obtain earthquake parameters. From the same data, a set of epicentral intensity-to-magnitude relations has been derived, with the aim of providing another set of homogeneous Mw estimates. Then, a strategy focussed on maximizing the homogeneity of the final epicentral location and Mw, has been adopted. Special care has been devoted also to supply location and Mw uncertainty. The paper focuses on the procedure adopted for the compilation of SHEEC and briefly comments on the achieved results.

Authors:
Craiu M., Craiu A., Ionescu C., Popa M., Radulian M.

Abstract:
The purpose of this paper is to revise the local magnitude formula for the intermediate-depth Vrancea earthquakes. The new magnitude scale is based on the local magnitude scale defined by [9] and revised by [3]. The coefficients in the magnitude relation is determined through multiple regression method using as reference the duration magnitude scale previously used in routine magnitude estimation for the earthquakes that occurred on the Romania territory. The amplitude (A) was measured on the horizontal components of broadband seismograms filtered to reproduce synthetically Wood-Anderson seismograms (in millimeters).

Authors:
Oros E.

Abstract:
Zona Timişoara este situată în centrul Regiunii Seismice Banat, cea mai importantă regiune seismică a României, dacă ne raportăm la hazardul seismic controlat de cutremure crustale (adâncimea focarelor mai mică de cca 30 km). Istoria seismică a zonei este marcată de seisme cu magnitudini maxime Mw = 5.6, care au provocat daune materiale semnificative fondului construit, atât în municipiul Timişoara cât şi în localităţile învecinate. Seismicitatea zonei este caracterizată prin grupări ale epicentrelor în arii bine definite, corelate cu un complex sistem de falii crustale rectivate într-un regim tectonic transtensiv. Seismele produse în perioada Ianuarie-Februrie 2012 confirmă caracterul seismic activ al sistemului de falii geologice dezvoltat în apropierea oraşului Timişoara şi importanta acestuia pentru evaluarea şi reducerea hazardului şi riscului seismic al oraşului Timişoara şi al localitaţilor invecinate acestuia. Pentru perioade de recurenţă specifice codurilor antiseismice national (P-100/2006) şi european (Eurocode EC8) hazardul seismic al zonei seismogene Timişoara este definit de intensitatea I = 7.0 EMS şi respectiv I = 7.5 EMS.

Authors:
Raileanu V., Tataru D., Grecu B., Bala A.

Abstract:
A new crustal model for the central and north-eastern parts of Romania is relying on the largest database available at this moment. In comparison with previous crustal models, the new model takes into account all known data: old and new seismic refraction data, deep seismic reflection data, and seismology data recorded by the broadband stations belonging to the Romanian seismic network for monitoring earthquakes. The new crustal model reveals the topography of the Moho and the top of the lower crust discontinuities as well as the areal distribution of the mean P-wave seismic velocities across the Moldavian and Scythian platforms and partially for the Eastern Carpathians. The new configuration of the Moho topography map brings some details to the central study area.

Authors:
Ren Y., Stuart G.W., Houseman G.A., Dando B., Ionescu C., Hegedus E., Radovanovic S., Shen Y., South Carpathian Project Working Group

Abstract:
The Carpathian–Pannonian system of Eastern and Central Europe represents a unique opportunity to study the interaction between surface tectonic processes involving convergence, extension, and convective overturn in the upper mantle. Here, we present high-resolution images of the upper mantle structure beneath the region from P-wave finite-frequency teleseismic tomography to help constrain such geodynamical interactions. We have selected earthquakes with a magnitude greater than 5.5 in the distance range 301–951, which occurred between 2006 and 2011. The data were recorded on 54 temporary stations deployed by the South Carpathian Project (2009–2011), 56 temporary stations deployed by the Carpathian Basins Project (2005–2007), and 131 national network broadband stations. The P-wave relative arrival times are measured in two frequency bands (0.5–2.0 Hz and 0.1–0.5 Hz) and are inverted for Vp perturbation maps in the upper mantle. Our images show a sub-vertical slab of fast material beneath the eastern Alps which extends eastward across the Pannonian basin at depths below 300 km. The fast material extends down into the mantle transition zone (MTZ), where it spreads out beneath the entire basin. Above 300 km, the upper mantle below the Pannonian basin is dominated by relatively slow velocities, the largest of which extends down to 200 km. We suggest that cold mantle lithospheric downwelling occurred below the Pannonian Basin before detaching in the mid-Miocene. In the Vrancea Zone of SE Romania, intermediate-depth (75–180 km) seismicity occurs at the NE end of an upper mantle high-velocity structure that extends SW under the Moesian Platform, oblique to the southern edge of the South Carpathians. At greater depths (180–400 km), a sub-circular high-velocity anomaly is found directly beneath the seismicity. This sub-vertical high-velocity body is bounded by slow anomalies to the NW and SE, which extend down to the top of the MTZ. No clear evidence of a residual slab is observed above the MTZ beneath the Eastern Carpathians. These observations suggest that intermediate-depth seismicity in Vrancea Zone is unlikely to be due to slab tearing, but rather could be explained by either gravitational instability or delamination of mantle lithosphere.

Authors:
Apostol B. F.

Abstract:
The electromagnetic field scattered by a rough surface of a semi-infinite body is computed up to the second order of a perturbation scheme with the surface roughness as a perturbation parameter. The calculations are basedon the equation of motion of the polarization within the Lorentz–Drude (plasma) model of polarizable,non-magnetic, homogeneous matter. The surface roughness contributes both to the main (specularly) reflectedand refracted fields and diffuse scattering, or gives rise to secondary (second-order) diffraction peaks for a regular grating. The calculations are performed both for the s- and p-waves. Two-dimensional modes, resonant at certain frequencies, are identified, confined to, and propagating only on the surface, as a consequence of the surface roughness.

Authors:
Zoran M., Savastru R., Savastru D., Chitaru C., Baschir L., Tautan M.

Abstract:
South-Eastern part of Romania has a highestpotential seismic risk in Europe due to the earthquakeproneVrancea zone placed at conjunction of four tectonicblocks in the South-Eastern part of Carpathian Arc. Thispaper is an attempt to analyze the development of radonpre-earthquake anomaly in relation with moderate seismicevents in Vrancea area through permanent monitoring withsolid state nuclear track detectors CR-39 detectors. Radonin air above the ground was measured during 1 year period(November 2010–October 2011) in four selected test sites:Vrancioaia (VRI) and Plostina (PLOR) located in Vranceazone, and Muntele Rosu-Cheia and Bucharest. Duringsampling period recorded earthquakes that occurred mostlyin Vrancea epicentral region were minor-moderate ofmoment magnitudes in range of 2:0 Mw 4:9. Theaverage radon concentration in air above the ground measuredwith CR-39 detectors and 10 days period recordedsimultaneously at all test sites, registered the followingvalues: (1) in Vrancea area (similar in VRI and PLOR) was1094.58 150.3 Bq/m3; (2) at Muntele Rosu-Cheia seismicstation measured in a mountain tunnel laboratory was3695.91 ± 440 Bq/m3; (3) at Bucharest station was380.53 69.17 Bq/m3, and 10 days CRn fluctuations in therange of (88 40 to 912 130 Bq/m3). Clear radonanomalies, mostly at VRI and PLOR in Vrancea epicentralarea as well as at Muntele Rosu-Cheia have been measuredbefore seven minor earthquakes which were recorded in therange of moment magnitude 4 Mw 4:9 in Vrancea area.Temporal variation of radon in air near the ground havebeen examined in relation with meteorological parameterslike as air temperature, relative humidity, air pressure andwind velocity. Permanent monitoring of radon concentrationanomalies in seismic area Vrancea is an importantissue as surveillance tool in the field of earthquake hazardfor Romania.Keywords Radon concentrations SSNTD CR-39 Vrancea seismic zone Romania

Authors:
Popa M.,Radulian M.,Szakacs A.,Seghedi I.,Zaharia B.

Abstract:
The southern part of the southeastern Carpathiansrepresents the site of the most recent volcanic eruptions of theentire Carpathian-Pannonian region. The products of these eruptionsrange from 42 to 10 Ka radiocarbon ages in the SouthHarghita Mountains (high K calc-alkaline rocks with adakite-likefeatures), and at 1.2–0.6 Ma K–Ar ages in the Pers¸ani Mountains(alkali basalts). They were emplaced in a post-collisional regime.Ciomadul volcano is located at the southernmost part of the NW–SE oriented Ca˘limani-Gurghiu-Harghita range crossing the innerpart of the southeastern Carpathians and in the rough proximity ofthe Vrancea seismic zone (at ca. 60 km toward NW). Its magmageneration is attributed to geodynamic events closely related to theseismogenic area. A number of particular geophysical and geochemicalfeatures located in the study region, including (1) theabrupt attenuation of the seismic waves originating from theVrancea intermediate-depth foci, (2) the most intense heat-flowanomaly in Romania, (3) the most prominent 3He/4He anomalymeasured in natural ‘‘postvolcanic’’ gas emanations, are all in favorof the hypothesis of a still existing hot local magma chamber. Dataacquired during recent seismic monitoring of the Vrancea zone andits neighborhoods suggest an enhancement of the local seismicitybeneath the southern edge of the South Harghita Mts., both atcrustal and subcrustal levels. At the same time, recent tomographyimages obtained using local earthquake data correlate well with thepresence of a vertically extended low-velocity zone coming fromthe upper mantle to the assumed magmatic chambers located in thecrust. The present data, supporting the presence of an active crustalmagma chamber beneath Ciomadul, allow us to consider that futurevolcanic activity at this volcano cannot be discarded.

Authors:
Panaiotu C.G.,Visan M.,Tugui A.,Seghedi I.,Panaiotu A.G.

Abstract:
Lavas of Pliocene-Quaternary age were sampled in the South Harghita Mountains which formthe southern end of the Calimani-Gurghiu-Harghita volcanic chain of the East Carpathians. Theanalyses of 68 volcanic sites in the South Harghita Mountains provided 62 sites with wellconstraineddirectional data (n> 5 and k > 50) and ages ranging from 0.5 to 4. 3 Ma. The age andpolarity for the 62 sites (38 normal and 24 reversed) are consistent with the GeomagneticReversal Time Scale and support the model of the south migration of the volcanism. Thedistribution of the VGPs is Fisherian and the mean pole position, both from all contributing sitesand from the 53 sites older than 2 Ma, includes the spin axis. This result is consistent with theabsence of important vertical axis rotations after the emplacement of the volcanic rocks inagreement with tectonic models for the Pliocene-Quaternary evolution of the bending area of theEast Carpathians. Virtual geomagnetic pole dispersions are consistently high compared withglobal values obtained between 40°N – 55°N, but closer to the values obtained only from theTime Averaged geomagnetic Field Initiative studies for the same latitudinal band. Our data arecompatible with the prediction of the statistical paleosecular variation model TK03. Theinclination anomaly is less than 1° in accord with the Total Average Field global data. Thesepaleomagnetic data from the South Harghita volcanic rocks are the first data from the southeasternEurope which can be considered in the databases for time averaged field and paleosecularvariation from lavas analyses in the last 5 Ma.

Authors:
Ismail-Zadeh A.,Matenco L.,Radulian M.,Cloetingh S.,Panza G. F.

Abstract:
The Vrancea region of the south-eastern Carpathians is a remarkable site of intra-continental intermediatedepthseismicity. A large set of geological, geophysical, and geodetic observations has been accumulated forthe last few decades and utilised to improve our knowledge of the shallow and deep structures beneath Vrancea,the crustal and mantle dynamics, and the linkage between deep and surface processes in the region. In thisarticle we review geology and tectonics of the Vrancea region including post-collisional to recent deformations,syn- to post-collisional magmatism, and orogenic exhumation along the East and South Carpathians.The regional seismicity is analysed, and the recent seismic studies including reflection, refraction, body andsurface wave tomography are reviewed. We discuss new geodetic measurements of horizontal and verticalmovements in the region, geoelectric studies, density/gravity and thermal modelling. Qualitative and quantitative(including retrospective) geodynamic models developed for Vrancea are analysed. The knowledge of regionaltectonics, geodynamics, seismicity, lithospheric deformation, and stress regime in the Vranceaearthquake-prone region assists in an assessment of strong ground motion, seismic hazard and risk. The earthquakesimulation, seismic hazard, and earthquake forecasting models have also been reviewed providing alink between deep geodynamic processes and their manifestation on the surface. Finally we discuss unresolvedproblems in Vrancea in order to improve our understanding of the regional evolution, present tectonics,mantle dynamics, intermediate-depth seismicity, and surface manifestations of the lithosphere dynamicsand to enhance our ability to forecast strong earthquakes in the Vrancea region. The problems to be solved include:(i) the origin of the high-velocity body revealed by seismic tomography studies (oceanic versus continental);(ii) the lithospheric scale mechanism driving the Miocene subsidence of the Transylvania basin;(iii) sub-crustal structure between 40 and 70 km; (iv) contemporary regional horizontal and vertical movements;and (v) a comprehensive seismic hazard assessment in the region.

Authors:
Borleanu F., Popa M., Radulian M., Schweitzer J.

Abstract:
The BURAR seismic array, located in Northern Romania (Bucovina region), is designed to monitor events located in an area poorly covered by other existing seismic stations. In order to use the BURAR array for single-station locations, it is crucial to calibrate the azimuth and slowness parameters, which are currently used in array techniques to locate earthquakes, blasts or nuclear explosions. The goal of this study is to apply “f–k” and plane wave fit techniques in order to constrain the slowness and azimuth parameters at BURAR for teleseismic, regional and local events. The analysis was carried out using P and S waves recorded for events occurred between 2004 and 2008 within a radius of 50◦ around BURAR. The azimuth values obtained applying both methods strongly deviated from the theoretical values for regions like Central Turkey, Bulgaria, Dodecanese Islands and other parts of Greece, while the ray parameter deviations with respect to a 1-D IASP91 reference model are less significant. For the local events, the anomalies are smaller, except the particular case of Vrancea intermediatedepth earthquakes for which strong azimuth deviations (33.5◦), both positive and negative, are observed. We investigate how these systematic deviations in azimuth are explained by the structure lateral heterogeneities which characterize the study region.

Authors:
Balan S. F., Apostol B. F.

Abstract:
A method for local effects estimation is employed here consisting in combining laboratory and in situ test performance, which implies the nonlinear modeling of geodynamical parameters of the soils. The two material functions, dynamic modulus function and damping function are computed here for materials which characterize the selected seismic areas. To accomplish this aim we use geodynamical profiles containing wave velocity measurements and resonant columns tests are performed. The differences between physical variables and natural conditions that influenced the initial values of the dynamic functions and the shape of the nonlinear variation curves are taking into account.

Authors:
Mateciuc D.

Abstract:
The author presents some observations on horizontal and vertical displacements recorded in a geodetic network located on Vrancea seismic zone. The fundamental differences between the displacement field from the northern part of the network in comparison with the southern part are pointed out.

Authors:
Mateciuc D., Malita Z.

Abstract:
he authors make a brief overview of the main features related to Vrancea zone seismicity and the earthquakes focal mechanism that can occur in the most important seismic region of Romania.

Authors:
Grecu B., Raileanu V., Bala A., Tataru D.

Abstract:
The purpose of our study is to investigate the ground motion characteristics in 15 sites located in the Eastern part of Romania by applying the H/V spectral ratio method to the data (S and coda waves) recorded during the CALIXTO’99 tomography experiment. The results show no significant differences as regarding the resonant frequencies of the spectral ratios computed for the two types of waves, while the level of the amplification for S-wave is slightly higher than for coda waves. Only for two sites, located on thick Quaternary deposits, the amplification obtained from S-wave is larger by a factor of 2 than the amplification obtained from coda waves at low frequencies. In the studied locations the ground motion amplification varies by a factor of 2 to nearly 6 over the frequency range of 0.5 to 10-12 Hz

Authors:
Ghica D.

Abstract:
Data recorded with the Bucovina Romanian Seismic Array (BURAR) seismic array between January 2005 and December 2008 were analyzed to verify the monitoring capabilities of regional and distant seismicity. For this time interval, nearly 35,000 events detected by BURAR and identified in seismic bulletins (Preliminary Determination of Epicenters and Romanian Earthquake Catalogue) were investigated using parameters as backazimuth, epicentral distance and magnitude. A remarkably detection capability is emphasized for teleseismic observations ( > 20â—¦). BURAR onsets could be associated to almost 60% of all events in the teleseismic distance, with a magnitude detection threshold of 4.5 (mb). When no threshold magnitude is applied, the full detection capability of BURAR is in the same order as the performance of GERES array, which is one of the most sensitive stations in Central Europe. For regional events, detection capability decreases to about 16% of all events within regional distance range. The site conditions (crustal structure and high frequency cultural noise) as well as array dimension, affect the signal coherency and reduce the array detection capability for regional events. For both teleseismic and regional distances, a monthly variation of BURAR detection capabilities has been found; the number of events detected during the summer time is diminished by the specific seasonal human activity and atmospheric conditions (thunderstorms). To prove the good detection capability of the BURAR for teleseismic distances, a comparison with the observations of the Romanian Real Time Network in terms of magnitude and epicentral distance was carried out. The higher signal detection capability of BURAR is due to the array techniques applied in data processing, which enhance the signal-to-noise ratio. The monitoring performed by the BURAR seismic array provides a good azimuthal coverage of the regional and distant seismicity, in a large range of epicentral distances.

Authors:
Bala A., Hannich D., Ritter J.R.R., Ciugudean T.V.

Abstract:
he local surface geology, the soil behaviour as well as the local hydrogeological factors have a well-known influence upon the characteristics of the earthquake ground motion and the corresponding site effects. The geological and hydrogeological setting in Bucharest, the capital of Romania, as well as relative short recurrence intervals of strong intermediate-depth earthquakes in the Vrancea area, make necessary to study the geological cause of observed seismic site effects. In the case of Bucharest, the source geometry of the intermediate-depth Vrancea earthquakes remains almost the same in respect to the city area, the hypocentral distances being in the range of 160–220 km, while the epicentral distances for Bucharest are in the range of 100–130 km. Compared to these distances the spatial extend of Bucharest – of about 20 km is small. Influences due to source directivity and travel path effects can be assumed to be constant over the entire city area. In the latest moderate earthquakes recorded peak ground accelerations varied over the city area by a factor of up to 4. The high ground motions recorded across Bucharest during strong earthquakes in the past result from sitespecific amplification within the city, obviously due to lateral variation of local soil and hydrogeologic near-surface conditions. To study this correlation it was necessary to know the geotechnical and dynamic properties of the involved geological layers.

Authors:
Moldovan I. A., Moldovan A. S., Ionescu C.

Abstract:
The paper presents the infrasound monitoring network installed at Plostina site, its characteristics and observations regarding its detection capability. Plostina is located at 45.8512 N latitude and 26.6499 E longitude in the Vrancea (Romania) epicentral zone, is characterized by a low infrasound noise background (due to the fact that is located far from cultural sources of acoustic perturbations) and is one of the most modern monitoring sites under the administration of the National Institute for Earth Physics (NIEP). Starting with July 2006, NIEP, AZEL – Designing Group S.R.L. and Bucharest University (BU) joined in a research consortium who’s project – Complex Multidisciplinary Research System On Precursory Phenomena Associated With Strong Intermediate Vrancea Earthquakes, In Conformity With The Latest International Approaches – MEMFIS – was financed by the Romanian Ministry of Research and Education, through the Program Excellency Research and had as a final purpose a new and modern geophysical monitoring network, that uses specific instruments providing information on acoustic (both earth's seismic and atmosphere's infrasonic activities), electric, magnetic and electromagnetic fields to find the correlations between monitored fields and the preparatory stage of strong intermediate earthquakes in Vrancea zone. Different connections between the activity of the acoustic field and other geophysical fields are presented, as well.

Authors:
Mateciuc D.

Abstract:

Authors:
Marmureanu G., Cioflan C.O., Marmureanu A.

Abstract:
The last zonation seismic map has areas where seismic intensities are underevaluated (e.g. Dobrogea, Banat etc.), and other areas are over-evaluated. The fundamental unacceptable point of view is that this design code is in peak ground accelerations which generates a lot of drawbacks to civil structural designers and to insurance companies which are paying all damages and causalities in function of earthquake intensity. The mapping is carried out using probabilistic approach and a complex hybrid waveform modeling method which combines the modal summation technique with finite-difference one to describe the seismic waves propagation through an inelastic space from source to free field surface. The result is a new seismic map in intensities by using probabilistic and deterministic approaches, linear and nonlinear seismology and developing the concept of control earthquake to obtain the banana shape of the attenuations curves of the macroseismic intensity along the directions defined by azimuths.

Authors:
Ardeleanu L.

Abstract:
The source parameters of low magnitude shallow earthquakes occurred in the Vrancea region and surroundings were previously estimated using an inversion procedure for high frequency local waveforms. Anticipating a gross approximation of the complex structure from the study area by the 1-D crustal models used in the forward modeling, the paper aims to assess the reliability of the resolved focal mechanism and source time function by stability tests which investigate the effect of hypocenter mislocation, mismodeling of the crust, frequency content of the inverted waveforms, and internal damping of the inversion algorithm on the retrieved solution. The analysis reveals that the over-simplification of the medium structure generates large uncertainties of the inverted source parameters, consequently not all the parameters may be accepted as sufficiently accurate. The most vulnerable is the source time function. The individual moment tensor components exhibit also poor resolution. By contrast, the double couple part of the moment tensor is determined fairly well, so that it allows correlations of the tension and pressure axes with the stress field in the area

Authors:
Constantin A. P., Pantea A., Stoica R.

Abstract:
The aim of the present paper is that of bringing in additional information regarding the macroseismic effects of the historical earthquakes that occurred on the Romanian territory with the purpose of improving the macroseismic maps. It is known the fact that in time, the Romanian territory has been shaken by strong earthquakes, most of them being centered within Vrancea Zone, which is situated at the bending zone of the South-Eastern Carpathians. As results from the contemporaries’ notes, such major earthquakes occurred also during the 19th century, on the 26th of October 1802 and the 23rd of January 1838, causing numerous victims and major material damages. Additional information that refer to the macroseismic effects produced by the above mentioned earthquakes, have been recently discovered due to the investigation of old books fund which exists in some monasteries and museums. The results of the investigation were concretized in discovering 37 historical records that allowed us to make a correct interpretation of the destroying impact of these earthquakes over the society and the environment. New elements regarding the research of these earthquakes were obtained after reevaluating the information from certain areas (especially from the epicentral zone), concerning the environmental effects. In this paper, the information referring to these earthquakes, identified as a result of investigating historical sources, are interpreted and evaluated with the purpose of assigning some seismic intensities for elaborating the macroseismic maps.

Authors:
Carbunar O. F., Radulian M.

Abstract:
For a seismogenic area like Vrancea (Romania) with well-defined geometrical features of the seismicity production in space and time, the numerical simulation of the earthquake generation process (e.g. cellular automaton) looks highly attractive. The delimitation, as accurately as possible, of the geometrical features of the seismically active system in the Vrancea subcrustal zone is essential to constrain the simulation modeling. As a first approximation, the seismicity pattern is close to a fault plane NE–SW oriented, extended roughly vertically between 60 and 170 km depth. A characteristic median plane is defined by minimizing the distance of hypocenters. The average distance of the hypocenters to the median plane is around 5 km. However, a more detailed investigation of the geometrical configuration of seismicity indicates a fragmentation of the active body located in the upper mantle in two segments.The seismicity pattern is well approximated by a planar distribution in each segment. In the transition zone, between the upper and lower segment, the hypocenter distribution is more dispersed and shows a disruption among the two planar segments, measured by about 9 km apart laterally one relative to the other. The two segments hosted the major Vrancea events recorded in the last two centuries (for which we have available location of acceptable accuracy). The narrow transition zone at about 100 km depth is interpreted as a weaker segment, possibly caused by a dehydration process or by an infiltration of asthenosphere material from the back side of the South-Eastern Carpathian arc system. It is still debatable if fragmentation in two seismically active segments reflects the existence of two neighbouring separate blocks (upper, continental and lower, oceanic block) or a consequence of a breaking process separating a continental block into two parts. The segmentation of the descending lithosphere and the edge effects are apparently stationary, at least for the time interval since 1985 to the present, for which the earthquake catalogue is reliable (homogeneous).

Authors:
Popescu E., Neagoe C., Rogozea M., Moldovan I. A., Borleanu F., Radulian M.

Abstract:
We applied relative deconvolution methods (spectral ratios and empirical Green’s function) to estimate the source parameters for the earthquake sequence recorded in the Ramnicu Sarat area between 29 November and 3 December 2007. Basically, these methods are suitable for seismic sequences since they allow the retrieve of the source parameters by using data from pairs of earthquakes located close each other and recorded by common stations. Our analysis reveals distinct features compatible with previous investigations, such as the alignment of the aftershocks parallel to the Carpathians Arc bend in the Vrancea region (NE-SW). The focal mechanism shows a rupture plane in the same direction as well. The location of the main shock relative to the aftershocks indicates a unilateral rupture, from SW toward NE. The alignment of the aftershocks in the sequence of 2007 (N30oE) is approaching the alignments observed in the sequences of 1991 (N24oE) and 1997 (N37oE). The values of the source parameters are typical for the earthquakes in the Vrancea foredeep area.

Authors:
Pantea A., Constantin A.P.

Abstract:
In order to set the basis of some rigorous standards and norms of antiseismic design, capable of assuring maximum security to buildings, in accordance with the idea of promoting and developing a national system, compatible with the European standardizing systems, we initiated a very large research activity especially of reevaluating and harmonizing of the macroseismic maps of the significant earthquakes occurred on the Romanian territory [9], [10], [11]. In this paper there have been reevaluated the macroseismic effects of the strongest vrancean earthquake occurred at 10th of November 1940. The reevaluating operation of the macroseismic data consisted in the reinterpretation of over 4500 macroseismic questionnaires, as well as the critical and serious research of the expertise reports, monographies, photos, scientific papers published both inside and outside the country regarding the severity of the macroseismic effects that were noticed “in situ” in the damaged areas. Taking into consideration the geological and tectonic complexity, as well as the distribution of the seismic active areas on the Romanian territory and in the transborder areas that influence the seismicity, we considered that it is necessary, for a better graphic representation of the distribution of the macroseismic field generated by the earthquake from the 10th of November 1940, to give up to the classical method of elaborating the isoseismal maps based on the smoothing operation of the excessively agitated isoseists.

Authors:
Neagoe C., Manea L.M., Ionescu C.

Abstract:
In 2002, the National Institute for Earth Physics started the development of its own real-time digital seismic network. This now consists of 86 seismic stations, of which 32 are broad-band sensors, 52 stations are equipped with short-period sensors, and two seismic arrays, all of which transmit data in real time to the National Data Center (NDC) and the Eforie Nord (EFOR) seismic observatory. EFOR is the back-up for the NDC, and it is also a monitoring center for Black Sea tsunamis. The seismic stations are equipped with Quanterra Q330 and K2 digitizers, broad-band seismometers (STS2, CMG40T, CMG 3ESP, CMG3T) and Episensor Kinemetrics acceleration sensors (±2g). SeedLink is a part of Seiscomp2.5 and Antelope, which are the software packages used for data acquisition in real time and data exchange. Communication from the digital seismic stations to the NDC in Bucharest and EFOR is assured by five providers (GPRS, VPN, satellite, radio and internet). AntelopeTM 4.11 is used for acquisition and data processing at these two data centers for the reception and processing of the data, which runs on two workstations: one for real-time processing and the other for offline processing. A Seiscomp 3 server works as the back-up for the Antelope 4.11. This acquisition and analysis systems for the seismic data produce information about the local and global parameters of earthquakes. In addition, Antelope is used for manual processing (e.g. association events, creation of a database, sending seismic bulletins, and calculation of magnitude and peak ground acceleration and velocity), generation of ShakeMap products, and interactions with global data centers. The NDC has developed tools to make all of this information easily available across the internet, and also to lay the grounds for a more modular and flexible development environment. This will enable centralizing of the data from software such as Antelope, which is using a dedicated database system (Datascope; a database system based on text files), to the more general-purpose database, MySQL. This acts like a hub between the different acquisition and analysis systems used at the NDC, while also providing better connectivity at no expense to security. Mirroring certain data to MySQL also allows the NDC to easily share information with the public, via the new application that is being developed, and also to mix in data collected from the public (e.g. information about the damage after an earthquake, which can be used to produce macroseismic intensity indices that are then stored in the database and also made available via the web application). For internal use, there is also a web application that uses the data stored in the database to display earthquake information, like location, magnitude and depth, in semi real time, thus aiding the personnel on duty. Another use for the data collected is to create and maintain contact lists to which the datacenter sends notifications (SMS and email), based on the parameters of an earthquake. For the future development, one of the NDC plans is to develop the means to cross-check the data generated between the different acquisition and analysis systems (e.g. comparing data generated by Antelope with data generated by Seiscomp).

Authors:
Marmureanu A., Ionescu C., Cioflan C.O.

Abstract:
The Vrancea seismogenic zone in Romania represents a peculiar source of seismic hazard, which is amajor concern in Europe, especially to neighboring regions of Bulgaria, Serbia and Republic of Moldavia. Earthquakes in the Carpathian–Pannonian region are confined to the crust, except the Vrancea zone, where earthquakes with focal depth down to 200 kmoccur. One of the citiesmost affected by earthquakes in Europe is Bucharest. Situated at 140–170 km distance from Vrancea epicenter zone, Bucharest encountered many damages due to high energy Vrancea intermediate-depth earthquakes; the March 4, 1977 event (Mw¼7.2) produced the collapse of 36 buildings with 8–12 levels, while more than 150 old buildings were seriously damaged. A dedicated set of applications and a method to rapidly estimate magnitude in 4–5 s from detection of P wave in the epicenter were developed. They were tested on all recorded data. The magnitude error for 77.9% of total considered events is in the interval [ 0.3, +0.3] magnitude units. This is acceptable taking into account that the magnitude is computed from only 3 stations in a 5 s time interval (1 s delay is caused by data packing). The ability to rapidly estimate the earthquake magnitude combined with powerful real-time software, as parts of an early warning system, allows us to send earthquake warning to Bucharest in real time, in about 5 s after detection in the epicenter. This allows 20–27 s warning time to automatically issue preventive actions at the warned facility.

Authors:
Ivan M.

Abstract:
Crustal thickness (CT) in Vrancea region (Romania) and adjacent area is investigated using 1294 S to P converted waves from the Moho discontinuity. A total of 269 local earthquakes in the depth range 99.8 to 171.1 km and recorded by 76 permanent and 46 temporary stations of the Romanian Seismological Network are used. Time difference between the converted wave and the direct P phase is corrected to a first order for epicentral distance and for the errors in focal depth, being finally inverted to CT. Greatest values for the Moho depth are observed for stations located in the Carpathians molasse foredeep and smaller values are observed in the Southern part of the Moesian Platform, for stations in the eastern part of Moldavian (East-European) Platform and in Dobrogea area, close to the Black Sea shoreline. In Vrancea epicentral area, an important CT variation is observed, from 42 km at MLR and 41.8 km at SIR, stations placed in the southwestern part of the epicentral area, to 30.9 km at VRI, located above north-eastern part of the seismogenic volume. Stations CVO and OZU, placed in Transylvanian Basin in the proximity of the epicentral area, have CT values of 32.1 and 24.1 km, respectively. The results seem to support that a mantle delamination process is responsible for Vrancea intermediate depth seismicity.

Authors:
Ivan M., Cormier V. F.

Abstract:
Anomalous high frequency PKKPBC signals (displaying a large amount of energy around 2.5 Hz), recorded globally for deep and intermediate depth earthquakes, are compared to PKKPAB signals. The attenuation difference t AB t BC is evaluated from spectral amplitudes in the range 96–111 , being approximately twice the results provided by full-wave theory and PREM (with no low Ql zone in the lowermost mantle and a nearly infinite QK in the outer core). Most ray paths for such recordings are piercing the D00 region in the proximity of regions where ultra-low velocity zones (ULVZ) have been previously reported beneath the North Atlantic Ocean, the Southwest Pacific and the southwestern part of South America. If BC amplitudes around 2.5 Hz and at low frequencies (0.5–1.5 Hz) are comparable, the observed attenuation difference (in the frequency range 0.2–2.5 Hz) is small (around 0.25 s) and close to the PREM value. The particle motion of the high-frequency PKKPBC at 2.5 Hz is quite similar to that of the raw recording, suggesting a deep source. An explanation for this might be scattering of the BC branch in some very restricted areas of the lowermost mantle. Alternately, the presence of a thin layer with high attenuation in the D00 region would most likely be associated with either the ultra-low velocity zone (ULVZ) or light sediments on the underside of the core-mantle boundary (CMB). Correlated to other methods to investigate the lowermost mantle, the high-frequency PKKPBC can be used to map lateral variations of attenuation above the CMB, possibly associated with the boundary of the superplumes, especially when PKKPAB is observed.

Authors:
Grecu B., Tataru D., Raileanu V., Neagoe C.

Abstract:
It has been recently shown that correlations of seismic noise can carry deterministic information about the crust and upper mantle structure along the profile between two seismic stations. We studied the characteristics of the noise cross correlations between 3 Romanian broadband stations. We performed 23 hours-long cross correlations for the period of 5 years, and stacked them for every month of the year. We studied the seasonal variations of the noise cross correlation functions (NCFs) and we demonstrated that the amplitude of the NCFs is higher in winter than in summer. We applied the multiple filter technique (MFT - Dziewonski et al., 1969) to extract the group velocities of the surface wave fundamental-mode of the NCFs. Finally, we showed that, in case of similar travel paths, the dispersion curve of the Rayleigh wave generated by a crustal event and the dispersion curve of the NCF are comparable.

Authors:
Cioflan C. O., Marmureanu A., Marmureanu G.

Abstract:
Nonlinear effects in ground motion during large earthquakes have long been a controversial issue between seismologists and geotechnical engineers. Laboratory tests made by using resonant columns consistently show the reduction in shear modulus (G) and increase in damping ratio (D) with increasing shear strain (γ), i.e., G = G(γ), respectively, D = D(γ), therefore nonlinear viscoelastic constitutive laws are required.Aki [1] wrote: „Nonlinear amplification at sediments sites appears to be more pervasive than seismologists used to think…Any attempt at seismic zonation must take into account the local site condition and this nonlinear amplification”. In other words, the seismological detection of the nonlinear site effects requires a simultaneous understanding of the effects of earthquake source, propagation path and local geological site conditions. The difficulty for seismologists in demonstrating the nonlinear site effects has been due to the effect being overshadowed by the overall patterns of shock generation and propagation. The authors, in order to make evidence of nonlinear effects, introduced the spectral amplification factor (SAF) as ratio between maximum spectral absolute acceleration (Sa), relative velocity (Sv), relative displacement (Sd) and peak values of acceleration (amax), velocity (vmax) and displacement (dmax), respectively, from processed strong motion record. The evidence for nonlinearity at least for thick Romanian Plain Quaternary sediments is a systematic decrease in the variability of peak ground acceleration with the increasing earthquake magnitude.

Authors:
Ardeleanu L., Raileanu V.

Abstract:
The goal of this work is to test the capability of high frequency local waveform inversion to retrieve the source of low magnitude intermediate depth earthquakes of Vrancea region. Following a similar procedure to that previously developed to analyze the weak shallow events from the Eastern Carpathians bending zone, we obtain a fairly robust estimate of the orientation of the double couple component of the seismic moment tensor. The resolution of the resolved fault plane solution allows correlations with the stress field in the area; this opens perspectives to using the small subcrustal earthquakes, frequently recorded, to obtain detailed information on the process taking place in the Vrancea focal region.

Authors:
Marmureanu G., Cioflan C. O., Marmureanu A.

Abstract:
The Vrancea seismogenic zone in Romania denotes a peculiar source of seismic hazard, which represents a major concern in Eastern Europe, especially in neighboring regions from Bulgaria, Serbia, Republic of Moldova etc. The last seismic zonation map of Romania has areas where seismic intensities are under-evaluated (e.g. Dobrogea, Banat) and for other areas are over-evaluated. In this study the mapping of seismic hazard is carried out by a probabilistic approach starting from the strong motion records of the August 30, 1986 event (Mw=7.1) used here as etalon earthquake. A complex neo-deterministic approach based on computation of synthetic seismograms have been applied to evaluate the hazard related with the superficial seismic sources and for a strong earthquake scenario of the November 10, 1940 Vrancea event with Mw=7.5. The results of both probabilistic and deterministic analyses are combined in a new seismic zonation map presented here in terms of macroseismic intensities

Authors:
Gheorghita M., Suciu E., Moldovan A. S., Moldovan I. A.

Abstract:
The paper presents the testing results of a new VLF/LF receiver for seismic precursors’ monitoring in Romania that is used, starting with March 2009, in the first phase of the Integrated System for the Forecast of Earthquakes in the European area. The system aims to capitalize and integrate numerous research results related to the statistical provisioning of seismic events and is consisting of a network of measuring stations, interconnected and organized through a distributed information system, which can allow consistently the availability of data acquired continuously. The acquired data refer to the amplitude of signals received in Romania and transmitted by high-power VLF and LF transmitters located in Europe. The paper shows why anomalous changes of the received signal level occur as an effect of modification of the characteristics of the ionosphere above the epicenter of an earthquake which is in its preparatory stage, if this is located inside the 5th Fresnel zone of the propagation path. Changes of the ionosphere’s altitude and composition, recorded as electromagnetic propagation anomalies, could be regarded as seismic precursors. This is accomplished with the help of ground-based network of receivers and appropriately located transmitters. The main contribution of the paper is that experimental data containing recordings of VLF/LF electromagnetic field monitoring in Romania are presented for the first time. Moreover, these data are consistent with data recorded in other countries. Key words: VLF/LF antenna, VLF/LF receiver, seismic precursors, electromagnetic anomalies.

Authors:
Fillerup M. A., Knapp J. H., Knapp C. C., Raileanu V.

Abstract:
The Vrancea seismogenic zone of Romania is a steeply NW-dipping volume (30 × 70 × 200 km) of intermediate-depth seismicity in the upper mantle beneath the bend zone of the Eastern Carpathians. It is widely held that the source of this seismicity is the remnant of a Miocene-age subduction zone. However, recent deep seismic-refl ection data collected over the Eastern Carpathian bend zone image an orogen lacking (1) a crustal root and (2) dipping crustal-scale fabrics routinely imaged in modern and ancient subduction zones. Here, we use these data to evaluate the lithospheric structure of the Eastern Carpathians as it relates to the Vrancea seismogenic zone. Crustal architecture obtained from these data indicate the 140-km-wide orogen is only supported by ~33-km-thick crust, while the adjacent Transylvanian and Focsani basins have ~37- (possibly up to ~46 km) and 42-km-thick crust, respectively. Because the Vrancea seismogenic zone is located beneath the east side of the thin orogenic crust, we infer that the lower orogenic crust was removed through continental delamination and is now represented by the mantle seismicity observed in the Vrancea seismogenic zone. These data and their interpretation suggest an alternate means of generating mantle seismicity in the absence of subduction processes.

Authors:
Ionescu C., Dragoicea M.

Abstract:
Earthquakes that are unambiguously sensed by humans or even destructive are often happening natural phenomena in Romania. The MACROSEIS application is an automated tool for collecting information from volunteers that felt the effects of an earthquake. Based on this interactive system, data can be collected and macroseismic maps can be obtained. The MACROSEIS application collects reports from volunteers that were sent via Internet shortly after an event is produced. Electronic reports are sent to the National Institute for Earth Physics. This information is further transformed in CII Community Internet Intensity Maps by means of a modified version of the Dengler and Dewey algorithm.

Authors:
Apostol B. F.

Abstract:
A new method is introduced for studying the propagation of elastic waves in isotropic bodies, based on the Kirchhoff potentials borrowed from electromagnetism. By means of this method we identify and characterize the elastic waves generated in a semi-infinite (half-space) body by the action of an external force localized on, or beneath, the body surface. The method implies coupled integral equations for the wave amplitudes, which we solve for both cases mentioned above. For a force localized on the body surface we identify two transverse waves, corresponding to the two polarizations (normal and parallel to the propagation plane). The longitudinal waves appear as eigenmodes. The waves produced by a force localized beneath the surface are stationary waves along the normal to the surface. We compute the surface displacement in both cases and the force exerted on the surface by a force localized beneath. All these quantities exhibit a characteristic decrease with the distance on the body surface and an oscillatory behaviour. We discuss briefly some possibilities of extending the present method to include the effect of the inhomogeneities on the waves propagation.

Authors:
Apostol B. F.

Abstract:
A new method is introduced for estimating the effects of the inhomogeneities on the propagation of the elastic waves in isotropic bodies. The method is based on the Kirchhoff electromagnetic potentials. It is applied here for estimating the effect of a static density inhomogeneity, either extended or localized, on the elastic waves propagating in an infinite, or a semi-infinite (half-space) body. For a semi-infinite body the method leads to coupled integral equations, which are solved. It is shown that such a density inhomogeneity may renormalize the waves velocity, or may even produce dispersive waves, depending on the geometry of the body and the spatial extension of the inhomogeneity. The method can be extended to other types of geometries or inhomogeneities, as, for instance, those occurring in the elastic constants.

Authors:
Apostol B. F.

Abstract:
The propagation of elastic waves in isotropic bodies is investigated by a new method, based on the electromagnetic Kirchhoff potentials. This method is applied herein to elastic waves produced in a semi-8 infinite (half-space) isotropic body by the action of an external force localized beneath, or on the body surface. The method leads to coupled integral equations for the wave amplitudes, which are solved for the both cases. The waves produced by a force localized beneath the surface are stationary waves along the normal to the surface. For a force localized on the body surface two transverse waves are identified, corresponding to the two polarizations (normal and parallel to the propagation plane). Another longitudinal wave appears as an eigen-mode. The surface displacement and the force exerted on the surface are computed in both cases. All these quantities exhibit a characteristic decrease with the distance on the body surface and an oscillatory behaviour. A brief discussion is included regarding some possibilities of extending the present method to treating the effect of the inhomogeneities on the waves propagation.

Authors:
Cocco M., Hainzl S., Catalli F., Enescu B., Lombardi A.M., Woessner J.

Abstract:
We use the Dieterich (1994) physics‐based approach to simulate the spatiotemporal evolution of seismicity caused by stress changes applied to an infinite population of nucleating patches modeled through a rate‐ and state‐dependent friction law. According to this model, seismicity rate changes depend on the amplitude of stress perturbation, the physical constitutive properties of faults (represented by the parameter As), the stressing rate, and the background seismicity rate of the study area. In order to apply this model in a predictive manner, we need to understand the impact of physical model parameters and the correlations between them. First, we discuss different definitions of the reference seismicity rate and show their impact on the computed rate of earthquake production for the 1992 Landers earthquake sequence as a case study. Furthermore, we demonstrate that all model parameters are strongly correlated for physical and statistical reasons. We discuss this correlation, emphasizing that the estimations of the background seismicity rate, stressing rate, and As are strongly correlated to reproduce the observed aftershock productivity. Our analytically derived relation demonstrates the impact of these model parameters on the Omori‐like aftershock decay: the c value and the productivity of the Omori law, implying a p value smaller than or equal to 1. Finally, we discuss an optimal strategy to constrain model parameters for near‐real‐time forecasts.

Authors:
Koulakov, I., Zaharia B., Enescu B., Radulian M., Popa M., Parolai S., Zschau J.

Abstract:
Vrancea, located at the southeastern Carpathians Arc bend, is one of the areas in the Alpine-Himalayan belt that features strong earthquakes occurring at intermediate depths (60–200 km). In this study we investigated the crustal and lithospheric structure beneath the Vrancea seismic area using a local earthquake tomography approach. We used an updated and revised catalog, spanning from 1982 to 2006 that uses data from both permanent and temporary networks in the target area. Simultaneous tomographic inversion for the Vp and Vs anomalies and the Vp/Vs ratio and source locations was done using the LOTOS code. The reliability and robustness of the results were rigorously checked using various tests (e.g., by studying the role of different parameters on the results of the inversion, performing the inversion using random data subsets, and synthetic modeling). The tomography results clearly indicate the presence of a high-velocity material beneath Vrancea at a depth interval of about 60–200 km that coincides with the distribution of intermediate-depth seismicity. This result agrees generally with previous tomographic studies. We compare two scenarios leading to this structure: (1) subduction and slab detachment and (2) ‘‘drop forming’’ or delamination. The latter mechanism presumes that the thickening of the crust due to continent-continent collision causes transformation of the mafic lower crust into denser eclogite. This material accumulates until it reaches a critical mass, at which point it forms a large drop that begins to fall down. We propose that the high-velocity anomaly we observe in our tomogram might represent the descending eclogitic lower crust material enveloped by the entrained lithosphere. It is possible that a similar delamination process can be observed in other parts of the Alpine-Himalayan belt, such as in the Pamir Hindu-Kush area.

Authors:
Ganas A., Grecu B., Batsi E., Radulian M.

Abstract:
he purpose of this paper is to study the interaction of the Vrancea seismic activity (Romania) in space as result of Coulomb, static stress transfer duringM =7+ events. In this area, three large events occurred in 1977, 1986 and 1990 at mid-lower, lithospheric depths and with similar focal mechanisms. Assuming elastic rheology for the deforming rocks it is suggested that frictional sliding on pre-existing fault produced the 1986 M =7.1 event (depth 131 km), that was possibly triggered by the 1977 M = 7.4 event (depth 94 km). We calculated a static stress transfer of 0.52–0.78 bar to the hypocentre of the 1986 event. On the contrary, the occurrence of the 1990 event is uncertain: it is located inside the relaxed (shadow) zone of the combined 1977 and 1986 static stress field considering an azimuth for maximum compression of N307 E. It follows that, the 1990 earthquake most likely represents an unbroken patch (asperity) of the 1977 rupture plane that failed due to loading. However, if a different compression azimuth is assumed (N323 E) then the 1990 event was also possibly triggered by static stress transfer of the 1977 and 1986 events (combined). Our modeling is a first-order approximation of the kind of earthquake interaction we might expect at intermediate lithospheric depths (80–90 to 130–140 km). It is also suggested that static stress transfer may explain the clustering of Vrancea earthquakes in space by the rupturing of two (possibly three) NW-dipping major zones of weakness (faults) which accommodate the extension (vertical elongation) of the slab.

Authors:
Boudjada M. Y., Schwingenschuh K., Doeller R., Rohznoi A., Parrot M., Biagi P. F., Galopeau P.H.M., Solovieva M., Molchanov O., Biernat H.K., Stangl G., Lammer H., Moldovan I. A., Voller W., Ampferer M.

Abstract:
We investigate the VLF emissions observed by the Instrument Champ Electrique (ICE) experiment onboard the DEMETER micro-satellite. We analyze intensity level variation 10 days before and after the occurrence of l’Aquila earthquake (EQ). We found a clear decrease of the VLF received signal related to ionospheric whistler mode (mainly Chorus emission) and to signal transmitted by the DFY VLF station in Germany, few days (more than one week) before the earthquake. The VLF power spectral density decreases of more than two orders of magnitude until the EQ, and it recovers to normal levels just after the EQ occurrence. The geomagnetic activity is principally weak four days before EQ and increases again one day before l’Aquila seismic event. Our results are discussed in the frame of short- and longterms earthquakes prediction focusing on the crucial role of the magnetic field of the Earth.

Authors:
Popescu E., Borleanu F., Placinta A. O., Neagoe C., Radulian M.

Abstract:
For the present study we selected 126 earthquakes of moderate magnitudes (3.2 ≤ MD ≤ 6.2) occurred in the time interval 1997–2005 in the Vrancea seismic region at intermediate depths (62 ≤ h ≤ 166 km). Two relative deconvolution techniques (spectral ratios and empirical Green’s function) are applied to retrieve the source parameters. To this purpose, the data set was divided into pairs of main and empirical Green’s function events. We could select 28 main events and 98 empirical Green’s functions. Six main events are generated in the upper segment of the subducting lithosphere (60 ≤ h < 110 km) and twenty two in the lower one (h ≥ 110 km). In all cases, the signal/noise ratio as recorded by the Romanian seismic stations is acceptable for our purpose. Once the seismic source parameters (seismic moment, source dimension, stress drop) are estimated, we investigate the scaling properties for the Vrancea subcrustal source. A slight deviation from a homogeneous rupture process and significant variations on depth and on magnitude of the stress drop and source size are emphasized. They can be tentatively explained by a more efficient seismic energy release in the deeper segment of the subducting lithosphere and by the role played by fluids at intermediate depth.

Authors:
Neagoe C., Popa M., Diaconescu M., Radulian M.

Abstract:
The Vrancea seismic region represents a unique case of well-defined and intense intermediate-depth earthquake activity as a consequence of specific geodynamic processes at the continental contact between East-European, Moesian and Intra-Alpine plates. Apart the subcrustal earthquakes generated in the Vrancea slab, the analysis of seismicity puts into evidence two other clusters of subcrustal earthquakes (h > 50 km) toward the back-arc side of the SE Carpathians bend, one to the west (Sinaia), the other to the north-west (Bra¸sov Depression) relative to the Vrancea seismic source. The hypocenters lay down between 50 to 105 km in Sinaia and between 50 and 136 km in Bra¸sov Depression. The rate of seismic energy release is much lower (Mw ≤ 3.7 in Sinaia and Mw ≤ 3.1 in Bra¸sov Depression) than for Vrancea activity. The seismicity pattern in the SE Carpathians back-arc region upper mantle correlates well with the high-velocity structures depicted by seismic tomography investigations suggesting possible remnant deep lithospheric roots apart from the narrow well-defined slab generating Vrancea major earthquakes. The results outline significant lateral heterogeneities in the mantle and provide new data for incorporating seismological, geotectonic and volcanological data in a unified modeling of the complex processes taking place in the study region.

Authors:
Neagoe C., Ionescu C., Grecu B.

Abstract:

Authors:
Moldovan I. A., Moldovan A.S., Ionescu C., Panaiotu C.G.

Abstract:
The paper presents a complex geophysical monitoring and recording system, deployed in Romania, at Plostina observatory (4 sites: PLO1, PLO2, PLO3 and PLO4) and at Surlari site (SULR – Bucharest University). Plostina is located at 45.8512 N latitude and 26.6499 E longitude in the Vrancea (Romania) epicentral zone and is one of the most modern monitoring sites under the administration of the National Institute for Earth Physics (NIEP), Romania. Surlari is located at 44.6798 N latitude and 26.2543 E longitude, outside of the Vrancea epicentral zone, being under the administration of the Bucharest University (BU) and NIEP. Starting with July 2006, NIEP, AZEL – Designing Group S.R.L. and BU joined in a research consortium who’s project – “Complex Multidisciplinary Research System On Precursory Phenomena Associated With Strong Intermediate Vrancea Earthquakes, In Conformity With The Latest International Approaches – MEMFIS” – was financed by the Romanian Ministry of Research and Education, through the Programme “Excellency Research” and had as a final purpose a new and modern geophysical monitoring network, that uses specific instruments providing information on acoustic (both earth’s seismic and atmosphere’s infrasonic activities), electric, magnetic and electromagnetic fields. The main goal is to find the correlations between monitored fields and the preparatory stage of strong intermediate earthquakes in Vrancea zone. Key words: Earthquake forecast, electromagnetic and infrasonic monitoring, seismic precursors.

Authors:
Apostol B. F.

Abstract:
A new method is introduced for estimating the effects of the inhomogeneities on the propagation of the elastic waves in isotropic bodies. The method is based on the Kirchhoff electromagnetic potentials. It is applied here for estimating the effect of a static density inhomogeneity, either extended or localized, on the elastic waves propagating in an infinite, or a semi-infinite (half-space) body. For a semi-infinite body the method leads to coupled integral equations, which are solved. It is shown that such a density inhomogeneity may renormalize the waves velocity, or may even produce dispersive waves, depending on the geometry of the body and the spatial extension of the inhomogeneity. The method can be extended to other types of geometries or inhomogeneities, as, for instance, those occurring in the elastic constants.

Authors:
Moldovan I.A., Constantin A.P., Popescu E., Placinta A.O., Moldoveanu T.

Abstract:
Principalele rezultate ale acestei lucrări constau în evaluarea hazardului seismic datorat atât cutremurelor intermediare vrâncene, cât și cutremurelor crustale și în încadrarea în clase de risc seismic a tuturor barajelor din vestul Platformei Moesice. Rezultatele cercetărilor realizate în cadrul acestei lucrări și analiza datelor, dau autorităților și specialiștilor în construcții hidrotehnice informații privind modul în care barajeșe pot fi afectate în timpul producerii unui cutremur major, cu taote implicațiile referitoare la măsurile de protecție a populației și a bunurilor materiale. Scopul principal al lucrării devine astfel deplasarea de la acțiunile post-cutremur, care prevalează în prezent si care sunt deosebit de costisitoare, la acțiunile de prevenire, menite să creeze o bază științifică pentru luarea unor măsuri eficiente de reducere a pierderilor umane și materiale la cutremure.

Authors:
Cioflan C. O., Marmureanu A., Marmureanu G.

Abstract:
The seismic hazard of Romania has been the object of several studies based on probabilistic or deterministic methods (I). Details of the resulted hazard maps are still a controversial issue that leads to an innovative approach: a combined analysis of the available records and macroseismic information completed with numerical simulations since the strong motion records are rather scarce. The main purpose of this paper is to add new features regarding site effects evaluation and its role in seismic hazard analyses at regional and/or local scale. This study is focusing on nonlinear aspects of seismic ground motion and presents new results related to site effects induced by strong Vrancea intermediate events.

Authors:
Bratosin D., Balan F. S., Cioflan C. O

Abstract:
By numerical simulation using a nonlinear Kelvin-Voigt model, this paper propose a modeling method for resonant peaks dispersion provoked by nonlinear properties of the site materials. This method leads to a better approximation of the nonlinear dependence of dominant site periods, dependence with an important impact about site-structure resonance avoidance.

Authors:
Balan S. F., Radulescu F.

Abstract:
This paper intends to present physical characteristics of some sites scattered throughout Romanian territory. Field measurement tests (seismic and geotechnical) were performed on these sites. The following parameters were determined: seismic waves velocities (VP, VS), dynamic moduli values (longitudinal, Ed and shear, Gd), Poisson coefficient (d), apparent density (a), lithology and layer thickness. Laboratory tests on resonant columns (Drnevich) were performed on samples from almost the same sites. The shear modulus (Gd), shear velocity (VS) and apparent density (a) were determined for these samples (with known lithology and depths). Results from field and laboratory tests are analyzed, compared and discussed.

Authors:
Rogozea M., Popa M., Radulian M.

Abstract:
Seismicity of the Vrancea region shows characteristic clustering features in space, time and energy that are clearly related to specific physical processes in the subcrustal domain. For the study of the frequency-magnitude distribution and seismic cycle behaviour we use Romanian routine catalogue for a 100-year time interval (6589 events) as well as the historical catalogue and information. In the last 100 years, several seismic cycles can be identified in the Vrancea subcrustal domain. Earth cycle is characterized by a shock larger than 6.5 and a relative lack of earthquakes at intermediate magnitudes (around 6), which suggests a percolation-type process for the major shocks. A sort of balance for the seismic energy release between an upper active segment located around 90 km depth and a lower active segment located around 140 km depth seems to control the evolution of the successive cycles (at least for the last 100 years). We investigate the implications of the specific seismicity parameters in the two segments related to background and aftershock earthquake activities on the earthquake process evolution.

Authors:
Radulescu F.

Abstract:
Séismologie roumaine – repères historiques, scientifiques et humains. L’auteur a essayé de reconstituer l’évolution de la séismologie roumaine depuis le début (fin du XIXe siècle) jusqu’à nos jours. On présente les contributions des personnalités de marque dans le domaine: Ştefan Hepites, Mathei M. Drăghiceanu, Gheorghe Demetrescu, Ion Atanasiu, Gheorghe Petrescu, Liviu Constantinescu, Ion Cornea, Cornelius Radu et d’autres. On mentionne des éléments liés au developpement des appareils utilisés, les résultats des études des tremblements de terre, de la séismicité dans la croûte et dans le manteau supérieur sur le territoire roumain, ainsi que les résultats des études de microzonation et de séismologie.

Authors:
Marmureanu A.

Abstract:
Due to the huge amount of recorded data, an automatic procedure was developed and used to test different methods to rapidly evaluate earthquake magnitude from the first seconds of the P wave. In order to test all the algorithms involved in detection and rapid earthquake magnitude estimation, several tests were performed, in order to avoid false alarms. A special detection algorithm was developed, that is based on the classical STA/LTA algorithm and tuned for early warning purpose. A method to rapidly estimate magnitude in 4 seconds from detection of P wave in the epicenter is proposed. The method was tested on al recorded data, and the magnitude error determination is acceptable taking into account that it is computed from only 3 stations in a very short time interval.

Authors:
Moldovan I. A., Moldovan A. S., Panaiotu C. G., Placinta A. O., Marmureanu G.

Abstract:
The paper tries an association between an unexplained, slow evolving and significant amplitude geomagnetic anomaly and the Vrancea (Romania) October 2004 intermediate-depth earthquake of moderate-to-high magnitude (Mw=6.0) followed by few weaker earthquakes (Mw<3). The fact that previous studies of Vrancea seismogenic zone indicate that observable precursory anomalies in the geomagnetic impedance might precede intermediate Vrancea earthquakes of moment magnitudes Mw≥4.0 encouraged us to continue the researches in this direction and to improve both the research and the monitoring system. Key words: geomagnetic precursory anomaly, intermediate earthquakes.

Authors:
Hainzl S., Enescu B., Cocco M., Woessner J., Catalli F., Wang R., Roth F.

Abstract:
We discuss the impact of uncertainties in computed coseismic stress perturbations on the seismicity rate changes forecasted through a rate- and state-dependent frictional model. We aim to understand how the variability of Coulomb stress changes affects the correlation between predicted and observed changes in the rate of earthquake production. We use the aftershock activity following the 1992 M7.3 Landers (California) earthquake as a case study. To accomplish these tasks, we first analyze the variability of stress changes resulting from the use of different published slip distributions. We find that the standard deviation of the uncertainty is of the same size as the absolute stress change and that their ratio, the coefficient of variation (CV), is approximately constant in space. This uncertainty has a strong impact on the forecasted aftershock activity if a rate-and-state frictional model is considered. We use the early aftershocks to invert for friction parameters and the coefficient of variation by means of the maximum likelihood method. We show that, when the uncertainties are properly taken into account, the inversion yields stable results, which fit the spatiotemporal aftershock sequence. The analysis of the 1992 Landers sequence demonstrates that accounting for realistic uncertainties in stress changes strongly improves the correlation between modeled and observed seismicity rate changes. For this sequence, we measure a friction parameter Asn 0.017 MPa and a coefficient of stress variation CV = 0.95.

Authors:
Enciu D. M., Knapp C. C., Knapp J. H.

Abstract:
Integration of active and passive source seismic data is employed in order to study the nature of the relationships between crustal seismicity and geologic structures in the southeastern (SE) Carpathian foreland of Romania and the possible connection with the Vrancea Seismogenic Zone (VSZ) of intermediatedepth seismicity, one of the most active earthquakeprone areas in Europe. Crustal epicenters and focal mechanisms are correlated with four deep industry seismic profiles, the reprocessed Danube and Carpathian Integrated Action on Process in the Lithosphere and Neotectonics (DACIA PLAN) profile and the Deep Reflection Acquisition Constraining Unusual Lithospheric Activity II and III (DRACULA) profiles in order to understand the link between neotectonic foreland deformation and Vrancea mantle seismicity. Projection of crustal foreland hypocenters onto deep seismic profiles identifies several active crustal faults in the SE Carpathian foreland and suggests a mechanical coupling between the mantle located VSZ and the overlying foreland crust. The coupled associated deformation appears to take place on the Trotus Fault, the Sinaia Fault, and the newly detected Ialomita Fault. Seismic reflection imaging reveals the absence of west dipping reflectors in the crystalline crust and a slightly east dipping to horizontal Moho in the proximity of the Vrancea area. These findings argue against previously purported mechanisms to generate mantle seismicity in the VSZ including oceanic lithosphere subduction in place and oceanic slab break off, furthermore suggesting that the Vrancea seismogenic body is undetached from the overlying crust in the foreland.

Authors:
Bala A., Radulian M., Grecu B., Popescu E.

Abstract:

Authors:
Bala A., Grecu B., Ciugudean V., Raileanu V.

Abstract:
Bucharest is one of the cities most affected by earthquakes in Europe. Situated at 150–170 km distance from Vrancea epicentral zone, Bucharest had suffered many damages due to high energy Vrancea intermediate-depth earthquakes. For example, the 4 March 1977 event produced the collapse of 32 buildings with 8–12 levels, while more than 150 old buildings with 6–9 levels were seriously damaged. The studies done after this earthquake had shown the importance of the surface geological structure upon ground motion parameters. New seismic measurements are performed in Bucharest area aiming at defining better elastic and dynamic properties of the shallow sedimentary rocks. Down-hole seismic measurements were performed in a number of 10 cased boreholes drilled in the Bucharest City area. Processing and interpretation of the data lead to the conclusion that shallow sedimentary rocks can be considered weak in the area, down to 150–200 m depth. Seismic wave velocity values and bulk density values presented in the paper associated with local geology are useful primary data in the seismic microzonation of Bucharest City. They are used as 1D models to derive transfer functions and response spectra for the stack of sedimentary rocks in several parts of Bucharest area, leading to a better knowledge of the local site amplification and associated frequency spectra. In a recent study the H/V spectral ratio using Nakamura’s method was applied on the seismic noise measurements in 22 sites in Bucharest City in order to derive the fundamental period associated with these sites. The values confirm the previous results, showing a dominant resonance in the period range of 1.25–1.75 s. The fundamental periods obtained with Nakamura’s method are in good agreement with those computed on the basis of geological and geotechnical data in boreholes, which show an increase of the fundamental period in the Bucharest area from south to north, in the same direction as the increase of the thickness of the Quaternary deposits above the Fratesti layer which is considered the bedrock in the area.

Authors:
Enescu D

Abstract:
The application of the first method indicates that the next Vrancea earthquake (MW ≈ 6.7) will occur in the time period 2010–2011(?), or in the case 2012–2013(?), while according to the second method the major event would occur in the period 2018–2019. For this purpose, I use two alternative approaches based on the Benioff graphs and on the theory of Wiener filters, respectively.

Authors:
Zaharia B., Enescu B., Radulian M., Popa M., Koulakov I., Parolai S.

Abstract:
The main goal of this study is to investigate the lithospheric structure beneath Vrancea seismic area using local earthquakes. Vrancea area, located at the South-Eastern Carpathians Arc bend, is characterized by strong earthquakes generated at intermediate depths (60–170 km) in a complex geotectonic system. The tomography image resulted from teleseismic data (Martin et al., 2005; 2006) reveals a high-velocity body extended significantly beyond the seismic active zone in depth (going down to 400 km depth or even more), as well as laterally. An updated and revised catalog of 927 well-located events occurred between 1982 and 2006 in Vrancea and around was considered in the present study. The application of the tomography inversion for local events (Koulakov et al., 2007) allowed a notable increase of the resolution of the previous tomography image. The high-velocity body is strongly reduced in extension and practically mimics the distribution of hypocenters.

Authors:
Popa M., Radulian M., Mandrescu N., Paulescu D

Abstract:

Authors:
Oros E.

Abstract:
The investigation of the site-effects using spectral ratio methods in the city of Timisoara is presented. A non-reference-site technique, often called Nakamura’s method is used to determine the resonance frequencies, fr, of the uppermost sedimentary layers. The method was applied on i) seismic noise time-series (HVSRN); ii) earthquakes waveforms recorded by Timisoara Seismic Station (TIM). The resonance frequencies and H/V ratios amplitudes were mapped for a firstorder evaluation of site response and to emphasize lateral variations of the seismic ground motion as a microzonation main step. These frequencies were also correlated with the local geology, the observed macroseismic intensities in the city and with the theoretical fundamental frequencies of the buildings.

Authors:
Constantin A. P., Pantea A., Stoica R., Amarandei C., Stefan S.

Abstract:
The goal of the present paper is to enrich qualitatively and quantitatively the existing database about historical earthquakes occurred on the Romanian territory and in the adjacent areas by revaluating and completing it with new information obtained after some complex research activities. In this respect there were studied the old book funds existing in Bucharest, especially those from the religious and cultural institutions – monasteries, libraries, archives and museums, starting with the documents existing under the custody of the Romanian Patriarchy. For the beginning there were researched three thousand books appeared between 1683–1902 where there were found information about some earthquakes occurred between 1802 and 1913. By this research, there is achieved the extension in the past of the database regarding the seismicity of the Romania’s territory, by emphasizing seismic events that, according to some seismicity schemes, can repeat in the future, thus, being taken into account the major contribution of the historical seismicity to the seismic hazard assessment.

Authors:
Tugui A., Necula C., Panaiotu C.

Abstract:
Thermomagnetic curves, low field magnetic susceptibility variation, hysteresis parameters, FORC (first order reversal curves) diagrams were measured for representative samples from the main eruption phases in PerÅŸani Mountains. We found that magnetic mineralogy is dominated by the titanomagnetite series with grain size compatible with SD-MD mixture.

Authors:
Tugui A., Craiu M., Rogozea M., Popa M., Radulian M.

Abstract:
Vrancea seismic zone is located in Romania at the South-Easter Carpathians bend, where at least three major tectonic units are in contact: East Europen Plate, Intra-Alpine Plate and Moesian Plate. The seismicity of the Vrancea zone consist of both crustal and intermediate-depth earthquakes. The crustal events are moderate (Mw ≤ 5.5) and generally occur in clusters in space (the subzones Râmnicu Sărat and Vrâncioaia, situated in the Vrancea epicentral area and adjacent to it) and in time (main shocks accompanied by aftershocks and sometimes by foreshocks or swarms). Seismic activity in Râmnicu Sărat zone consist of shallow earthquakes with moderate magnitudes Ms ≤ 5.2 (Radu, 1979), wich frequently occur in clusters. The hypocenters are generally situated at focal depths between 15 and 30 km within the foredeep region lying in front of the major bending of the Carpatian Arc. The sequence of 29 November–03 December, 2007 consist of 37 events with 1.8 ≤ MD ≤ 3.9. The earthquakes hypocenters are grouped in a parallel direction with the Carpathian Bend, and the fault plane solution (of the main shock) is reverse. The seismic sequence from Râmnicu Sărat, 2007 was compared with the previous sequences knowing the regional seismotectonics.