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《Geology in China》 2008-05
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The surface rupture zone distribution of the Wenchuan earthquake (Ms8.0) happened on May 12th, 2008

LI Hai-bing1,2, WANG Zong-xiu3, FU Xiao-fang4, HOU Li-wei4, SI Jia-liang1,2, QIU Zhu-li1,2 , LI Ning5, WU Fu-yao1,2(1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;2. Key Laboratory for Continental Dynamics of the Ministry of Land Resources, Beijing 100037, China;3. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China;4. Academe of Geological Survey, Sichuan Province, Chengdu 610081, Sichuan China;5. 109 Geological Bridge, Sichuan Exploration and Development Bureau of Geology and Mineral Resources, Chengdu 610100, Sichuan China)  
On May 12, 2:28 pm, an earthquake (Ms 8.0) struck the Longmenshan area (centred in Wenchuan County of Sichuan Province), the eastern segment of the Tibetan Plateau. According to the field survey, the earthquake occurs on the NE striking Longmenshan fault belt. The belt has been with the thrusting rate smaller than 1 mm/a and the shortening rate smaller than 3 mm/a according to GPS measurement. The causative mechanism is mainly the thrust (from NW to SE), accompanied with dextral strike-slip. The earthquake produced several co-seismic surface rupture zones that were 275 km long and 15 km wide in general. The Yingxiu-Beichuan rupture zone is 275 km long and dominative;The Hanwang rupture zone takes the second place, which is 70 km long and occurs along the south part of the Guanxian-Anxian fault, the frontal fault of the Longmenshan fault belt. There are another two minor rupture zones between two zones mentioned above, one is the Shenxigou rupture zone, is in NE direction and about 10 km long, close to the southern segment of the main rupture zone, whose deformation characteristics are similar to and can be involved into the Yingxiu-Beichuan rupture zone; the other is named as Xiaoyudong rupture zone, is in NW direction and 6 km long, produced by the thrust from SW to NE and associated lateral slip, which is the link between Yingxiu-Beichuan and Hanwang rupture zone and characterized by the lateral ramp. Besides, in the Sichuan Basin that eastern to the Guanxian-Anxian fault, a sand liquefaction belt with NE direction strike developed from Juyuan town of Dujiangyan to Jiangyou, which might be the result of the activity of a blind fault deep in the western Sichuan Basin. According to the feature of surface coseismic rupture zones, active tectonics in the Longmenshan fault belt have intense thrusting accompanied with significant dextral strike-slip. The fault is developing toward the Sichuan Basin. The recurrence intervals of great earthquake such as the Wenchuan earthquake can be 3000-6000 years.
【Fund】: 中国地质调查局地质大调查项目(12010611811和10210610105)资助
【CateGory Index】: P315.2
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4 LI Yong 1 ,HOU Zhong-jian 1 ,SI Guang-ying 1 ,A.L.DENSMORE 2 ,ZHOU Rong-jun 3 ,M.A.ELLIS 4 ,LI Yong-zhao 1 ,LIANG Xing-zhong 1(1.Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu610059;Cenozoic tectonic sequence and tectonic events at the eastern margin of the Qinghai-Tibet plateau[J];Chinese Geology;2002-01
5 XU Zhi-qin, YANG Jing-sui, LI Hai-bing, ZHANG Jian-xin, ZENG Ling-sen, JIANG Mei (Key Laboratory for Continental Dynamics, MLR, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China);The Qinghai-Tibet plateau and continental dynamics: A review on terrain tectonics, collisional orogenesis, and processes and mechanisms for the rise of the plateau[J];Geology in China;2006-02
6 XU Zhi-qin~1, ZENG Ling-sen~1, YANG Jing-sui~1, LI Hai-bing~1, JIANG Mei~1, JIN Zhi-jun~2, ZHENG He-rong~2, GUO Qi-jun~2 1.Key Laboratory for Continental Dynamics, MLR, Institute of Geology, Chinese Academy of Geological Sciences, Beijing100037, China 2.China Petroleum and Chemical Corporation, Beijing100083, China;Role of Large-Scale Strike-Slip Faults in the Formation of Petroleum-Bearing Compressional Basin-Mountain Range Systems[J];;2004-06
7 ZHANG Dong-Ning~1,YUAN Song-Yong~1,SHEN Zheng-Kang~21 Institute of Geophysics,China Earthquake Administration,Beijing 100081,China2 Institute of Geology,China Earthquake Administration,Beijing 100029,China;Numerical simulation of the recent crust movement and the fault activities in Tibetan Plateau[J];Chinese Journal of Geophysics;2007-01
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 Chen Zhiliang; Liu Yuping; Zhang Xuanyang; Zhao Jixiang; Tang Wenqing;Deng Changrong; B. C. Burchfiel ;R.W. King ;L. H. Royden( Chengdu Institute of Geology and Mineral Resources , Chengdu 610082; Massachusetts Institute of Technology, Cambridge);GPS SURVEY AND THE RHEOLOGIC STRUCTURES WITH IN THE EASTERN TIBETAN PLATEAU[J];QUATERNARY SCIENCES;1998-03
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