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Rupture process of the Oct. 6, 2008 M(s)6.6 Damxung earthquake, Tibet, China
Gao Xing; Duan Zong-Qi; Wang Wei-Min; Guo Zhi
通讯作者Gao, X (通讯作者)
发表日期2010
ISSN0001-5733
起始页码2083
结束页码2090
卷号53期号:9
英文摘要The rupture process of the Oct. 6, 2008 Damxung earthquake (M(s)6.6) is studied by using the point source and finite fault model. The observed broadband seismograms used in the inversion were retrieved from DMC (Data Manager Center) of China Earthquake Networks Center (CENC) and of Incorporated Research Institute for Seismology (IRIS). Historical earthquake records indicated that this event is one of the strongest earthquakes in central Tibet in recent years, and its epicenter is located around the N-S trended Yadong-Golug rift zone in southern Tibet. Our inversion results show that the earthquake occurred on a west-dipping normal fault with the focal depth of 9.6 km, the fault plane has a strike of 183.3 degrees, a dip of 49.5 degrees. The rupture process lasted about 10 seconds with a maximum slip reaching 130 cm, consistent with a moment release of 2.84 x 10(18) N.m. The dynamic rupture process obtained in this study consists with the crustal movement obtained from GPS observations, implying that this earthquake was triggered by extension stress induced by transition of crustal movement from the direction of NNE to SSE from central southern Tibet to the eastern Himalaya Syntax.
关键词SOUTHERN TIBETQUATERNARY EXTENSIONSLIP HISTORYHECTOR MINECALIFORNIAPLATEAUTECTONICSCOLLISIONASIA
英文关键词The Tibetan Plateau; Damxung earthquake; Coseismic rupture; Waveform inversion; Simulated annealing method
语种英语
WOS研究方向Geochemistry & Geophysics
WOS类目Geochemistry & Geophysics
WOS记录号WOS:000282294600008
来源期刊CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/257745
推荐引用方式
GB/T 7714
Gao Xing,Duan Zong-Qi,Wang Wei-Min,et al. Rupture process of the Oct. 6, 2008 M(s)6.6 Damxung earthquake, Tibet, China[J]. 中国科学院青藏高原研究所,2010,53(9).
APA Gao Xing,Duan Zong-Qi,Wang Wei-Min,&Guo Zhi.(2010).Rupture process of the Oct. 6, 2008 M(s)6.6 Damxung earthquake, Tibet, China.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,53(9).
MLA Gao Xing,et al."Rupture process of the Oct. 6, 2008 M(s)6.6 Damxung earthquake, Tibet, China".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 53.9(2010).
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