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摘要:
Detecting tempo-spatial changes of crust stress associated with major earthquakes has implications for understanding earthquake seismogenic processes.We conducted a joint analysis of b-value and apparent stress in the source region before the March 11,2011 Mw9.0 Tohoku-Oki,Japan earthquake.Earthquakes that occurred between January 1,2000 and March 8,2011 were used to estimate b-values,while source parameters of events with magnitudes of Ms5.0-6.9 between January 1,1997 and March 8,2011 were used to calculate the apparent stresses.Our results show that the average b-value decreased steadily from 1.26 in 2003 to 0.99 before the Tohoku-Oki mainshock.This b-value decrease coincided with an increase in the apparent stress from 0.65 MPa to 1.64 MPa.Our results reveal a clear negative correlation between the decrease in b-value and increase in apparent stress,which lasted for approximately eight years prior to the 2011 mainshock.Additionally,spatial pattern results of the relative change in b-value show that the area associated with drastic b-value decreases(25%or greater)was concentrated near the 2011 mainshock epicenter.The joint analysis of b-value and apparent stress provides a promising method for detecting anomalies that could serve as potential indicators of large earthquakes.
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篇名 Joint analysis of b-value and apparent stress before the 2011 Mw9.0 Tohoku-Oki,Japan earthquake
来源期刊 地震学报(英文版) 学科
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年,卷(期) 2021,(4) 所属期刊栏目
研究方向 页码范围 323-333
页数 11页 分类号
字数 语种 英文
DOI 10.29382/eqs-2021-0036
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期刊影响力
地震学报(英文版)
双月刊
1674-4519
11-5695/P
16开
北京民族学院南路5号(北京8116信箱)
1980
eng
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1366
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