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《Chinese Journal of Geophysics》 2013-04
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The Lushan M_S7.0 earthquake on 20 April 2013:A high-angle thrust event

ZENG Xiang-Fang1,LUO Yan2,Han Li-Bo3,SHI Yao-Lin1 1 CAS Key Laboratory of Computational Geodynamics,University of Chinese Academy of Sciences,Beijing 100049,China 2 Institute of Earthquake Science,China Earthquake Administration,Beijing 100036,China 3 Institute of Geophysics,China Earthquake Administration,Beijing 100081,China  
P wave first motions picked from regional and teleseismic records were used to invert focal mechanism of the Lushan MS7.0 earthquake on 20 April 2013.To reduce errors introduced by uncertainties of take-off angle due to the velocity model and focal depth errors,random perturbations of take-off angle were added into raw values.After multiple trials,strike/dip/rake angles of the best solution are calculated to be 212°/44°/92°.To better understand focal mechanism,the regional and teleseismic waveforms inversion method(CAPjoint) was employed to determine the centroid depth,double-couple solution and magnitude.The results(212°/47°/93°,depth=12 km,Mw6.7) suggest that the Lushan earthquake is a high-angle thrust event.Both inversion results with three other seismic velocity models and focal mechanisms of short term aftershocks support this solution.
【Fund】: 国家自然科学基金项目(41204044)资助
【CateGory Index】: P315
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9 WANG Lian-jie1, LI Peng-wu2 , CUI Jun-wen2, DING Yuan-chen1 (1. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081,China; 2. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037,China));Determination of the present crustal stress state by using acoustic emission in the main borehole of the Chinese Continental Scientific Drilling[J];Chinese Geology;2005-02
10 SHI Yao lin (Graduate School, CAS, Beijing 100039, China);Stress triggers and stress shadows: How to apply these concepts to earthquake prediction[J];Earthquake;2001-03
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