Seismology is rated the Queen of Earth Sciences due to its ability to provide detailed structural information bearing on the Earth interior and on-going dynamic processes. This is due to the advanced theoretical foundation of seismology and the extensive cooperation among seismologists on recording and disseminating of data worldwide. In contrast, some 40 years ago seismology was a backward science and hence funding was poor.
This abruptly changed with the political interest in seismology as the principal tool for monitoring compliance with a potential Comprehensive Nuclear Test Ban treaty (CTBT) banning nuclear testing in any environment.
Major countries like USA, UK and USSR launched large-scale research programs including deployment of modern seismograph stations and arrays and these developments are detailed in the book for CTBTO (UN), IRIS (USA), MedNet (Italy), Geofon (Germany) and the tiny Karelia network, NW Russia. Station and network operations require near real time record analysis and topics dealt with here are 2-D signal detector, epicenter location and earthquake monitoring. Balkan is seismically the most active part of Europe due to multiple plate interactions in the Aegean Sea. The tectonic evolution and on-going geodynamic deformations are described in 2 articles. Earthquake hazard analysis and topographic site effects are discussed and likewise large earthquake hazards in the Aegean and the Marmara seas relate to practical applications of such procedures. Foremost; the book gives a good account of past, present and likely future seismological developments in Balkan countries and various kinds of network operations on local to global scales.
Author(s): Eystein S. Husebye
Series: NATO Science Series: IV: Earth and Environmental Sciences
Edition: 1
Publisher: Springer
Year: 2008
Language: English
Pages: 293
City: Dordrecht
Contents......Page 6
Foreword......Page 9
List of Sponsors, Scientific Directors, Organizing Committees......Page 12
List of Participants......Page 13
Part I: Tectonic Framework and Geodynamics of the South Balkan Region......Page 17
Patterns of Cenozoic Extensional Tectonism in the South Balkan Extensional System......Page 18
Crustal Motion and Strain Accumulation in the South Balkan Region Inferred from GPS Measurements......Page 34
Part II: Seismicity Studies in the South Balkan Region......Page 59
Recent Devastating Earthquakes in Turkey and Active Tectonics of the Aegean and Marmara Seas......Page 60
Estimates of Stress Drop and High Frequency Diminution Parameter from Strong Motion Data Recorded in Albania......Page 69
Seismicity of Croatia......Page 92
Seismicity of the Pannonian Basin......Page 110
Part III: Seismic Network Operations on Global, Regional and National Scales......Page 122
The CTBTO International Monitoring System and Global Seismicity......Page 123
The IRIS Consortium: Community Based Facilities and Data Management for Seismology......Page 131
The Mediterranean Broad Band Seismographic Network Anno 2005/06......Page 143
GEOFON and its Role in Earthquake Monitoring and Tsunami Warning......Page 160
The Karelian Regional Seismic Network in NW Russia......Page 172
Part IV: Seismic Network Operations, Event Location and 2-D Signal Detection......Page 178
Cossack Ranger II – A High Quality, Versatile and Affordable 3-Component Short-Period Seismograph......Page 179
A 2-D Seismic Signal Detector for Stand Alone 3-Component stations......Page 196
Accurate Location of Seismic Sources With and Without Travel Time Model......Page 204
Earthworm Auto-Earthquake Location Performance and Recent Improvements in Seismic Data Acquisition, Processing, Archiving and Dissemination at Kandilli Observatory and Earthquake Research Institute......Page 224
Part V: Seismic Hazard Analysis and Assessment......Page 241
Data Driven Probabilistic Seismic Hazard Assessment Procedure for Regions with Uncertain Seimogenic Zones......Page 242
Seismicity and Seismic Hazard Assessment in Greece......Page 257
Are Rock Avalanches and Landslides Due to Large Earthquakes or Local Topographic Effects? A Case Study of the Lurøy Earthquake of August 31, 1819, A 3D Finite Difference Approach......Page 275
