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  1. Acta Geodaetica et Geophysica Hungarica
  2. Acta Geodaetica et Geophysica Hungarica : Volume 43
  3. Acta Geodaetica et Geophysica Hungarica : Volume 43, Issue 2-3, June 2008
  4. Romanian Seismic Network development
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Acta Geodaetica et Geophysica Hungarica : Volume 52
Acta Geodaetica et Geophysica Hungarica : Volume 51
Acta Geodaetica et Geophysica Hungarica : Volume 50
Acta Geodaetica et Geophysica Hungarica : Volume 49
Acta Geodaetica et Geophysica Hungarica : Volume 48
Acta Geodaetica et Geophysica Hungarica : Volume 47
Acta Geodaetica et Geophysica Hungarica : Volume 46
Acta Geodaetica et Geophysica Hungarica : Volume 45
Acta Geodaetica et Geophysica Hungarica : Volume 44
Acta Geodaetica et Geophysica Hungarica : Volume 43
Acta Geodaetica et Geophysica Hungarica : Volume 43, Issue 4, December 2008
Acta Geodaetica et Geophysica Hungarica : Volume 43, Issue 2-3, June 2008
Preface
Evidence of strong lateral inhomogeneous structure beneath SE Carpathians and specific mantle flow patterns
Spatial and temporal variations of the correlation coefficient between M2 and S2 earth tides components and earthquake occurrences for the intermediate-depth seismic activity zones
Romanian Seismic Network development
Review of the historical seismicity in the western and southwestern territory of Romania (Banat Seismic Region)
Seismicity patterns in Vrancea and predictive features
Inversion of the October 27, 2004 Vrancea (Romania) earthquake using teleseismic waveforms data
Thermal models simulating the tectonic processes in the extra-Carpathian area (on the Romanian territory): rheological models and their interpretation in relation with the local seismic wave attenuation models
Seismotectonic modeling for seismic hazard analysis of Vardar zone in Republic of Macedonia
Evaluation of PGA for Tirana city
Analysis of strong motion data from three events (M $_{W}$ = 4.3–4.9) recorded recently in central Albania area
An approach of Microzonation of the Sofia city
Estimation of an upper limit on prehistoric peak ground acceleration using the parameters of intact speleothems in caves situated at the western part of Balkan Mountain Range, North-West Bulgaria
Ground motion models — State of the art
History of early isoseismal maps
Fragility evaluation of existing typified school buildings in Albania
Some remarks on the seismic risk to lifelines, with references to the activity of the Vrancea seismogenic zone
Seismic safety of structures — Case study: Probabilistic methodological approach to definition of seismic input
Synthesis of nonstationary seismic response of structures
Simulation and analysis of seismic response of a structure for Sofia region with synthetic accelerograms
Acta Geodaetica et Geophysica Hungarica : Volume 43, Issue 1, March 2008
Acta Geodaetica et Geophysica Hungarica : Volume 42
Acta Geodaetica et Geophysica Hungarica : Volume 41
Acta Geodaetica et Geophysica Hungarica : Volume 40
Acta Geodaetica et Geophysica Hungarica : Volume 39
Acta Geodaetica et Geophysica Hungarica : Volume 38
Acta Geodaetica et Geophysica Hungarica : Volume 37
Acta Geodaetica et Geophysica Hungarica : Volume 36
Acta Geodaetica et Geophysica Hungarica : Volume 35
Acta Geodaetica et Geophysica Hungarica : Volume 34
Acta Geodaetica et Geophysica Hungarica : Volume 33
Acta Geodaetica et Geophysica Hungarica : Volume 32

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Romanian Seismic Network development

Content Provider Springer Nature Link
Author Neagoe, C. Ionescu, C.
Copyright Year 2008
Abstract The Romanian Seismic Network consisting of 8 short-period stations (S13), 60 Altus — K2 and Q330 seismic stations, is primarily designed to survey the Vrancea seismic region (strong and moderate Vrancea earthquakes). Since July 2002, a new seismic monitoring system, Bucovina Seismic Array (BURAR) has been operating. BURAR consists of 12 seismic stations distributed on a 5 km × 5 km area. 9 stations are equipped with short-period (SP) vertical sensors (GS-21 res) and one station is equipped with broad-band (BB) three component sensor (KS 54000). Broad-band sensors GMG40T (1000V/cm/s) were installed at 5 of the short-period stations, at the beginning of 2008. Recently, NIEP has developed its real-time digital seismic network. This network consists of 21 broad band stations and one seismic array. In the next year NIEP will install additional broad band stations in the central part of Romanian territory and other 40 strong motions stations in Bucharest.At the National Data Centre (NDC) runs BRTT’s Antelope™ 4.9 data acquisition and processing software on two HP workstations for real-time and post processing. The Antelope Real-Time System is also providing automatic event detection, arrival picking, event location and magnitude calculation.The Romanian Seismic Network is already linked with IRIS and ORFEUS organizations and other European countries via Internet and is contributing in near real time with waveform data from 5 broadband stations.The seismotectonic characteristics of the Vrancea region offer the opportunity to create and develop a rapid seismic warning system. This system allows warning in an approximately 25 seconds time window for Bucharest.
Starting Page 145
Ending Page 152
Page Count 8
File Format PDF
ISSN 12178977
Journal Acta Geodaetica et Geophysica Hungarica
Volume Number 43
Issue Number 2-3
e-ISSN 15871037
Language English
Publisher Springer Netherlands
Publisher Date 2013-02-27
Publisher Institution Quarterly of the Hungarian Academy of Sciences
Publisher Place Dordrecht
Access Restriction Subscribed
Subject Keyword seismic stations automatic event detection seismic monitoring warning system real-time processing sensor Geophysics/Geodesy
Content Type Text
Resource Type Article
Subject Building and Construction Geology Geophysics
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