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《Chinese Journal of Geophysics》 2013-04
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Preliminary result for rupture process of Apr.20,2013,Lushan Earthquake,Sichuan,China

WANG Wei-Min 1,HAO Jin-Lai 2,YAO Zhen-Xing 2 1 Key Laboratory of Continental Collision and Plateau Uplift(LCPU),Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing100101,China 2 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing100029,China  
The rupture process of the 20,Apr.2013,Lushan earthquake was fast estimated by finite fault model method using far field body waveform records.The predicted shakemap is subsequently calculated based on rupture fault model of this earthquake.Results show that the earthquake is an Mw6.7 thrusting event which occurred on the south part of Longmen Shan fault zone with 159 cm largest slip.By the predicted shakemap,the intensity of epicenter region should reached Ⅷ—Ⅸ on Chinese seismic intensity scale.The thrusting mechanism of Lushan earthquake is similar to that of Wenchuan earthquake.The earthquake rupture of this event occurred on the southern section of Longmen Shan fault where shows increase of Coulomb stress caused by the Wenchuan earthquake.This event may be triggered by the Wenchuan earthquake.On the view of macroscopic,this earthquake can be considered as an delayed strong aftershock of Wenchuan earthquake.
【Fund】: 国家自然科学基金项目(41030319 41174037 41202049)资助
【CateGory Index】: P315
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8 HE Ri-Zheng 1,2 ,GAO Rui1,ZHENG Hong-Wei 1,3 ,ZHANG Ji-Sheng11 Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China2 Geo-detection Laboratory, Ministry of Education of China, China University of Geosciences, Beijing 100083, China3 Geophysical Department, Peking University, Beijing 100871, China;Matched-filter analysis of aeromagnetic anomaly in mid-western Tibetan Plateau and its tectonic implications[J];Chinese Journal of Geophysics;2007-04
9 QIAN Hui~1,JIANG Mei~1,CHEN Wang-Ping~2,John Nabelek~3,ZHAO Da-Peng~4,ZHAO Lei~1,WANG Ya-Jun~1 1 Key Laboratory for Continental Dynamics of the Ministry of Land and Resources of China,Institute of Geology,Chinese Academy of Geological Science,Beijing 100037,China2 Dept.Geology,Univ.of Illinois,1310 W.Green St.,Urbana,IL 61801,United States3 College Ocean.Atm.Sci.,Oregon State University,Corvallis,OR 97331-550,United States4 Geodynamics Research Center,Ehime University,Matsuyama 790-8577,Japan;Tomography of Gyirong-Lugu profile(Hi-Climb) and the subduction of Indian-Tibet collision[J];Chinese Journal of Geophysics;2007-05
10 SHAO Zhi-Gang1,2,FU Rong-Shan1,XUE Ting-Xiao1,HUANG Jian-Hua1 1 Key Laboratory of Crust-Mantle Materials and Environments,Chinese Academy of Sciences,Hefei 230026,China 2 College of Earth and Space Sciences,University of Science and Technology of China,Beijing 100036,China;The numerical simulation and discussion on mechanism of postseismic deformation after Kunlun M_s 8.1 earthquake[J];Chinese Journal of Geophysics;2008-03
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