Journal of Seismology

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Adaptation of P-wave moment magnitude of Turkey’s earthquakes for early warning purpose
Journal of Seismology - Tập 26 - Trang 243-263 - 2022
Timur Tezel
The determination of an earthquake’s magnitude correctly is vital to understand the situation and prevent loss of lives and planning first organization for the rescue with early warning/tsunami warning at a region. In this study, we calculated moment magnitude using a P-wave portion of seismic records and indicated that it is possible to use it with all available seismic data recorded at local and...... hiện toàn bộ
Correction to: Microtremor array method using spatial autocorrelation analysis of Rayleigh-wave data
Journal of Seismology - - 2022
Koichi Hayashi, Michael W. Asten, William J. Stephenson, Cécile Cornou, Manuel Hobiger, Marco Pilz, Hiroaki Yamanaka
Instructions for authors
Journal of Seismology - Tập 7 - Trang 139-143 - 2003
Peculiarities of Rayleigh wave displacement in a transversely isotropic half space
Journal of Seismology - - 2018
S. N. Bhattacharya
Stochastic finite fault modelling of M w 4.8 earthquake in Kachchh, Gujarat, India
Journal of Seismology - Tập 16 - Trang 435-449 - 2012
Sumer Chopra, Dinesh Kumar, Pallabee Choudhury, R. B. S. Yadav
The modified stochastic finite fault modelling technique based on dynamic corner frequency has been used to simulate the strong ground motions of M w 4.8 earthquake in the Kachchh region of Gujarat, India. The accelerograms have been simulated for 14 strong motion accelerographs sites (11 sites in Kachchh and three sites in Saurashtra) where the earthquake has been recorded. The re...... hiện toàn bộ
On the cessation of seismicity at the base of the transition zone
Journal of Seismology - Tập 2 - Trang 377-381 - 1998
Active surface faulting or landsliding in the Lower Tagus Valley (Portugal)? A solved controversy concerning the Vila Chã de Ourique site
Journal of Seismology - Tập 15 - Trang 215-234 - 2010
João Manuel Cabral, Fernando Marques, Paula Figueiredo, Luís Matias
The Lower Tagus Valley has experienced significant (M 6–7) historical seismicity, evidencing the presence of seismogenic faults. These are still deficiently known due to the low strain rates and the recent alluvial sedimentation of the Tagus River that buries most of the structures, though Paleoseismic evidence was allegedly found by a research team in the Tagus valley, at a site 60 km N of Lisbon...... hiện toàn bộ
The Ms = 6.2, June 15, 1995 Aigion earthquake (Greece): evidence for low angle normal faulting in the Corinth rift
Journal of Seismology - - 1997
P. Bernard, P. Briole, B. Meyer, H. Lyon-Caen, J.-M. Gomez, C. Tiberi, C. Berge, R. Cattin, D. Hatzfeld, C. Lachet, B. Lebrun, A. Deschamps, F. Courboulex, C. Larroque, A. Rigo, D. Massonnet, P. Papadimitriou, J. Kassaras, D. Diagourtas, K. Makropoulos, G. Veis, E. Papazisi, C. Mitsakaki, V. Karakostas, E. Papadimitriou, D. Papanastassiou, M. Chouliaras, G. Stavrakakis
We present the results of a multidisciplinary study of the Ms = 6.2, 1995, June 15, Aigion earthquake (Gulf of Corinth, Greece). In order to constrain the rupture geometry, we used all available data from seismology (local, regional and teleseismic records of the mainshock and of aftershocks), geodesy (GPS and SAR interferometry), and tectonics. Part of these data were obtained during a postseismi...... hiện toàn bộ
Attenuation of P, S, and coda waves in Koyna region, India
Journal of Seismology - Tập 11 - Trang 327-344 - 2007
Babita Sharma, S. S. Teotia, Dinesh Kumar
The attenuation properties of the crust in the Koyna region of the Indian shield have been investigated using 164 seismograms from 37 local earthquakes that occurred in the region. The extended coda normalization method has been used to estimate the quality factors for P waves $$ {\left( {Q_{\alpha } } \right)} $$ ...... hiện toàn bộ
Evaluation of local site effect from microtremor measurements in Babol City, Iran
Journal of Seismology - Tập 22 - Trang 471-486 - 2017
Sadegh Rezaei, Asskar Janalizadeh Choobbasti
Every year, numerous casualties and a large deal of financial losses are incurred due to earthquake events. The losses incurred by an earthquake vary depending on local site effect. Therefore, in order to conquer drastic effects of an earthquake, one should evaluate urban districts in terms of the local site effect. One of the methods for evaluating the local site effect is microtremor measurement...... hiện toàn bộ
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