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《Seismology and Geology》 2008-04
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AN ANALYSIS ON M_S 8.0 WENCHUAN EARTHQUAKE FAULT AND SEISMIC DISASTER

ZHAO Bo-ming1)XU Xi-wei2)1)School of Civil Engineering,Beijing Jiaotong University,Beijing 100044,China2)National Center for Active Fault Studies,Institute of Geology,China Earthquake Administration,Beijing 100029,China  
Complex spatial distribution of seismic motion near faults has always been a concern to scientists,and it still remains as an uncertain problem due to insufficiency of events and information.The paper presents the main cases of seismic disaster by field investigations of MS 8.0 Wenchuan earthquake,analyzes and discusses the relationship among earthquake fault,ground motion and earthquake disaster near the fault fractured zone,based on previous research of source rupture processes and source inversion of Wenchuan earthquake.Intensive deformation and ground surface rupture along the earthquake fault have caused obvious damage to buildings,so it is necessary to introduce the safety distance away from active fault and other measures.Possible reasons for buildings near surface rupture zone having withstood the strong earthquake are as follows:other than their performance of seismic resistance,firstly,most of them locate at hard sites or on bedrock in the surface rupture zone,and secondly,the effective stress drop and low rupture velocity may exist in the shallow asperities,resulting in a relatively lower ground motion at the period about 1 sec.
【Fund】: 国家自然科学基金(40674016);; 科技部地震行业基金(2007203853);; 中国地震局汶川8.0级地震应急科学考察项目共同资助
【CateGory Index】: P315.2
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8 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
9 Li Yong~① Zhou Rongjun~② A.L.Densmore~③ M.A.Ellis~④(①State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu610059;②Institute of Earthquake Engineering,Seismological Bureau of Sichuan Province,Chengdu610041;③Institute of Geology,Department of Earth Sciences,ETH Zentrum,CH-8092 Zürich Switzerland;④Center for Earthquake Research and Information,( )University of Memphis,3890 Central Avenue,Memphis,TN 38152 USA);GEOMORPHIC EVIDENCE FOR THE LATE CENOZOIC STRIKE-SLIPPING AND THRUSTING IN LONGMEN MOUNTAIN AT THE EASTERN MARGIN OF THE TIBETAN PLATEAU[J];Quaternary Sciences;2006-01
10 ZHANG Pei-zhen 1, WANG Min 1,2 , GAN Wei-jun 1, DENG Qi-dong 1 (1.State Key Laboratory of Earthquake Dynamics, Institute of Geology, CSB, Beijing 100029, China; 2. Center for Analysis and Prediction, China Seismological Bureau, Beijing 100039, China);SLIP RATES ALONG MAJOR ACTIVE FAULTS FROM GPS MEASUREMENTS AND CONSTRAINTS ON CONTEMPORARY CONTINENTAL TECTONICS[J];Earth Science Frontiers;2003-S1
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