Retrospective analysis of seismic regime features before the Taiwan earthquakes of 1999 and 2002
- 作者: Kuzin I.P.1, Flyonov A.B.1
- 
							隶属关系: 
							- Shirshov Institute of Oceanology
 
- 期: 卷 56, 编号 3 (2016)
- 页面: 415-427
- 栏目: Marine Geology
- URL: https://journals.rcsi.science/0001-4370/article/view/149178
- DOI: https://doi.org/10.1134/S0001437016030127
- ID: 149178
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The features of the seismic regime before the strongest earthquakes of Taiwan in the late 20th (Chi-Chi on September 21, 1999, Mw = 7.6) and the early 21st century (March 31, 2002, Mw = 7.4) are analyzed. Based on 1990–1999 and 1994–2002 data, respectively, retrospective analysis of three seismic regime parameters are studied: the total annual number of earthquakes NΣ in the range of ML = 2.5–5.5 and Mw = 3.0–7.0; the total annual quantity of released seismic energy ΣE, J; and angular coefficient b of earthquake recurrence graphs. Two explicit subperiods are revealed in the course of the seismic regime: quiescence in 1990–1996 before the Chi-Chi earthquake and in 1994–1997 before the March 2002 earthquake; in 1997–1999 and 1998–2002, respectively, seismic activation is observed. Due to the predominance of weak earthquakes during the Chi-Chi earthquake preparation, factor b appeared relatively higher (–1.16 on average); in contrast, before the March 2002 earthquake, due to the occurrence of foreshocks with Mw = 6.8–7.0, the factor b values appeared relatively lower (–0.55 and–0.74 for the quiescence and activation subperiods, respectively). Despite the fundamental difference in the seismotectonic situation between the domains where two mainshocks occurred and significantly difference energy ranges of the initial seismic events, the analysis results are similar for both earthquakes. In both cases, the mainshock occurred at the peak of released energy, which can be considered a coincidence. Solid verification of this positive tendency requires the accumulation of seismological statistics.
作者简介
I. Kuzin
Shirshov Institute of Oceanology
							编辑信件的主要联系方式.
							Email: ivkuzin2013@yandex.ru
				                					                																			                												                	俄罗斯联邦, 							Moscow						
A. Flyonov
Shirshov Institute of Oceanology
														Email: ivkuzin2013@yandex.ru
				                					                																			                												                	俄罗斯联邦, 							Moscow						
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