Rupture process of the July 11, 2004, Tibet (M-w 6.2) earthquake
Li, J; Wang, WM; Zhao, LF; Yao, ZX
刊名CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
2005-07-01
卷号48期号:4页码:843-850
关键词Finite Fault Model Source Rupture Process Simulated-annealing Inversion
ISSN号0001-5733
文献子类Article
英文摘要The source rupture process of the July 11, 2004, Tibet (M-w 6. 2) earthquake is investigated by a finite fault model using far field broadband body wave records. The results show that it is a shallow dip-slipping predominant normal-fault earthquake, and the hypocentral. depth is about 12.5km. The fault plane has a strike of 152 degrees and a dip of 44 degrees, and the average slip angle is - 117 degrees. The rupture nucleates near the hypocenter, then propagates to the two ends of the fault with an average velocity of 2.8km/s, and the slip reaches to its maximum value of 43cm at about 5km northeast of the epicenter. The main principal T axis of the fault plane solution shows roughly EW extension, which is controlled by a local rift belt in NNW-SSE or nearly NS direction, and the thrust motion of the southern Tibetan plateau towards north is the main mechanical reason of this earthquake.
WOS关键词1999 HECTOR MINE ; 7.6 BHUJ ; CALIFORNIA ; INDIA ; INVERSION ; XINJIANG ; VELOCITY ; BENEATH ; MODELS ; CHINA
WOS研究方向Geochemistry & Geophysics
语种英语
出版者SCIENCE PRESS
WOS记录号WOS:000230837400016
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/65210]  
专题中国科学院地质与地球物理研究所
通讯作者Li, J
作者单位Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
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GB/T 7714
Li, J,Wang, WM,Zhao, LF,et al. Rupture process of the July 11, 2004, Tibet (M-w 6.2) earthquake[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2005,48(4):843-850.
APA Li, J,Wang, WM,Zhao, LF,&Yao, ZX.(2005).Rupture process of the July 11, 2004, Tibet (M-w 6.2) earthquake.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,48(4),843-850.
MLA Li, J,et al."Rupture process of the July 11, 2004, Tibet (M-w 6.2) earthquake".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 48.4(2005):843-850.
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