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《Chinese Journal of Geophysics》 2012-01
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Surface rupture features of the 2010 Yushu earthquake and its tectonic implication

SUN Xin-Zhe1,XU Xi-Wei1*,CHEN Li-Chun1,TAN Xi-Bin1,YU Gui-Hua1, LI Zhi-Min2,SU Gui-Wu1,WANG Ji3,ZHANG Xiao-Qing2 1 National Center for Active Fault Studies,Institute of Geology,China Earthquake Administration,Beijing 100029,China 2 Earthquake Administration of Qinghai Province,Xining 810001,China 3 China Earthquake Disaster Prevention Center,Beijing 100029,China  
Field investigations show that the Yushu,Qinghai Province,MS7.1 earthquake occurred on the Yushu segment of the Ganzê-Yushu fault in the Qinghai-Tibetan Plateau.Its surface rupture zone is distributed along the Yushu segment between Longbao Town and Jiegu Town and consists of shear cracks,transtensional cracks,transpressional cracks,tension cracks,mole tracks in right-stepovers or small pull-aparts in left-stepovers between en echelon cracks with left-lateral component.Those ruptures are en echelon to form an ~300°-striking earthquake surface rupture zone with a total length of about 65 km.The maximum co-seismic left-lateral displacement is 2.4 m.The width of the surface rupture zone is in general less than 30 m,showing a localized rupturing feature.The Yushu earthquake surface rupture zone can be divided into two relatively independent sections in left-step: the Jielong section ~15 km long with a maximum left-lateral slip of 0.66 m and Jiegu section ~ 31 km with a maximum left-lateral slip of 2.4 m,and between them is a 17 km-long-section where no surface ruptures occurred,which correspond to two subevents with MW6.4 and MW6.9,respectively.This kind of the surface rupture pattern shows that the Ganzê-Yushu fault,a seismogenic fault of the Yushu earthquake,is dominated by a pure left-lateral faulting and the eastward escape of the Qinghai-Tibetan Plateau exists.
【Fund】: 国家自然科学基金(40821160550和40974057);; 中国地震局玉树地震科学考察项目资助
【CateGory Index】: P315
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