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《Chinese Journal of Geophysics》 2014-02
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A preliminary study of seismogenic structure for the Xinyuan-Hejing,Xinjiang M_S6.6 earthquake of June 30,2012

LI Zhi-Hai;ZHENG Yong;XIE Zu-Jun;LIU Jian-Ming;SHANGGUAN Wen-Ming;SHAN Bin;Earthquake Administration of Xinjiang Uygur Autonomous Region;State Key Laboratory of Geodesy and Earth′s Dynamics,Institute of Geodesy and Geophysics,Chinese Academy of Sciences;  
On June 30,2012,an MS6.6earthquake occurred at the border between Xinyuan and Hejing counties,Xinjiang Uygur Autonomous Region.It is the largest earthquake between the M7.1Yushu,Qinghai Province event in 2010and the M7.0Lushan,Sichuan Province event in2013.Based on seismic phase data of the earthquake sequence recorded by the Xinjiang Digital Seismic Network,we relocated the MS6.6and its aftershocks by the absolute and relative locationmethods.The epicenter location of the mainshock is 43.429°N,84.755°E,the focal depth is 21.8km,and the aftershocks are distributed in NW direction.In terms of the waveforms of the M6.6earthquake,we used the CAP method to make a grid search for the focal mechanism and the focal depth.The resulting focal mechanism solution includes 39°,46°,12°for the strike,dip,and rake angles on one plane and 301°,81°,135°on the other plane,respectively,and a focal depth of 21km.So,the waveform inversion result is consistent with that by phase data.The strike and dip angles for the plane II of the focal mechanism solution are close to the Northern Edge fault of the Yili basin,and the relocated distribution of the aftershocks is also in agreement with the characteristics of the fault.Therefore,this fault should be the seismogenic structure of the Xinyuan-Hejing MS6.6earthquake,which is of high angle and dip-slip in nature.
【Fund】: 国家自然科学基金(41104037 41174086);; 地震公益性行业科研专项项目(201308013);; 地震科技星火计划(XH12055);; 湖北省自然科学杰出青年基金(2012FFA026);; 大地测量与地球动力学国家重点实验室开放基金(SKLGED2013-5-2-E);; 新源—和静6.6级地震科考课题联合资助
【CateGory Index】: P315
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