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《Journal of Geological Hazards and Environment Preservation》 2009-02
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MAIN TYPES AND CHARACTERISTICS OF THE GEO-HAZARDS TRIGGERED BY THE WENCHUAN EARTHQUAKE

XU Qiang(State Key Laboratory of Geohazard Prevention and Geoenvironment Protection,Chengdu University of Technology,Chengdu 610059,China)  
Great amount of geo-hazards have been triggered by the Wenchuan Earthquake on May 12,2008.It made a serious threaten to the properties of the people who live in those regions and it become a main factor which need to be considered during the remediation project after the earthquake.The paper based on lots of site-investigations of the regions and did some related indoor simulations to provide a systematic research on the main types and characteristic of earthquake triggered landslide,collapse,unstable slopes and debris flow.To conclude,the regions where the geo-hazards developed have a close relationship with the rock structures and the topography condition.The critical,initiate and slide phases of landslide were different when it occurred in hard rock region,soft rock region and the loose accumulation.In general,the movement has the characteristic of high speed,high energy released.The collapses which triggered by the earthquake can be distinguished into three types: the high altitude large collapse;the rock burst in small scale and the large landslide triggered by collapse.In the high magnitude earthquake,the rock burst always moved horizontally.There are also some cracked mountains after the strong shocks.It can be sub-distinguished into three types: cracks due to the broken rock,cracks due to the shaking affect and cracks due to the tension sliding.The quake also provide a large amount of loose materials for the future debris flow which become a great potential threaten to the upcoming remediation plan.Early warning should be given as well as the related counter measures.
【Fund】: 国家重点基础研究发展计划课题“强震作用下斜坡失稳破坏机理及分布规律”(2008CB425801);; 教育部创新团队项目“地质灾害评价预测理论与防治技术研究”联合资助
【CateGory Index】: P315;P694
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5 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
6 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
7 Song Hongbiao;Luo Zhili(Chengdu Institute of Technology,Chengdu,610059);THE STUDY OF THE BASEMENT AND DEEP GEOLO-GICAL STRUCTURES OF SICHUAN BASIN,CHINA[J];EARTH SCIENCE FRONTIERS;1995-04
8 Yang Xiaoping Jiang Pu Song Fengmin Liang Xiaohua Chen Xiancheng (Institute of Geology, China Seismological Bureau, Beijing 100029)Deng Zhongwen (Hydraulic and Electric Power Designing Institute of Sichuan, Chengdu 610000);THE EVIDENCE OF THE SOUTH LONGMENSHAN FAULT ZONES CUTTING LATE QUATERNARY STRATUM[J];SEISMOLOGY AND GEOLOGY;1999-04
9 Lü Jiang ning 1) SHEN Zheng kang 2) WANG Min 3) 1) Department of Geophysics, School of Earth and Space Science, Peking University, Beijing 100871, China 2) Institute of Geology, China Seismological Bureau, Beijing 100029, China 3) Center for Earthquake Analysis and Prediction, China Seismological Bureau, Beijing 100036, China;CONTEMPORARY CRUSTAL DEFORMATION AND ACTIVE TECTONIC BLOCK MODEL OF THE SICHUAN-YUNNAN REGION,CHINA[J];Seismology and Geology;2003-04
10 MA Bao-qi SU Gang HOU Zhi-hua SHU Sai-bing (Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China);LATE QUATERNARY SLIP RATE IN THE CENTRAL PART OF THE LONGMENSHAN FAULT ZONE FROM TERRACE DEFORMATION ALONG THE MINJIANG RIVER[J];Seismology and Geology;2005-02
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