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《Earth Science Frontiers》 2013-03
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Seismogenic structure of Lushan earthquake and its relationship with Wenchuan earthquake

XU Xiwei1,CHEN Guihua1,YU Guihua1,CHENG Jia1,TAN Xibin1, ZHU Ailan2,WEN Xueze3 1.Institute of Geology,China Earthquake Administration,Beijing 100029,China 2.Shanghai Earthquake Administration,Shanghai 201203,China 3.Sichuan Earthquake Administration,Chengdu 610041,China  
The Lushan earthquake occurred on the southern segment of the Longmenshan thrust belt between the Bayan Har and south China blocks.Field investigations indicated that there is no any earthquake surface rupture zone generated by this earthquake,only secondary surface breaks,such as extensional ground fissures,landslides,bedrock collapses,and liquefactions were found in the epicentral areas,which were caused by slope instability and earthquake vibration.The relocated aftershocks,focal mechanism solutions and surface structural geology further demonstrate that the seismogenic fault of the Lushan earthquake is a blind reverse fault which strikes 212° and dips toward NW with a dip angle of 38°±2°.The upper tip of this blind reverse fault is still at the depth of about 9 km in the upper crust.The structural deformation from above the tip to the ground surface is in accordance with a fault-propagation-anticline model.Besides,the differences in spatial aftershocks' distribution,rupturing process and seismogenic structure suggest that the Wenchuan and Lushan earthquakes are two independent rupturing events occurred along the middle segment and southern segment of the Longmenshan thrust belt,respectively.
【Fund】: 国家自然科学基金项目(40821160550 91214201);; 中国地震局芦山7.0级强烈地震科学考察项目
【CateGory Index】: P315
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10 XIONG SIIAO-BAI TENG JI-WBN YIN ZIIOU-XUNLAI MING-HUI HUANG YI-PING (Institute of Geophysics, Academia Sinica);EXPLOSION SEISMOLOGICAL STUDY OF THE STRUCTURE OF THE CRUST AND UPPER MANTLE AT SOUTHERN PART OF THE PANXI TECTONIC BELT[J];Chinese Journal of Geophysics;1986-03
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