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《Chinese Journal of Geophysics》 2009-01
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Relationships between surface ruptures and lithologic characteristics of the Wenchuan M_s 8.0 earthquake

WANG Ping1,FU Bi-Hong2,ZHANG Bin1,KONG Ping2,WANG Gang3 1 State Key Laboratory of Earthquake Dynamics,Institute of Geology,China Earthquake Administration,Beijing 100029,China2 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China3 College of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China  
Two co-seismic surface rupture zones,230 km and 70 km long,are produced by the 2008 Wenchuan Ms 8.0 earthquake along the pre-existing Yingxiu-Beichuan fault and the Guanxian-Anxian fault,respectively,in the Longmen Shan fault zone.The post-earthquake geological study shows that the exposed fault planes accompanying with co-seismic scarps usually occurred along the coal seams and carbonaceous shales.In this paper we present the observed results of fault scarps and the slip surface in some typical locations along the co-seismic rupture zones.Comparing with the 1:50000 regional geological map,it shows that the distribution of the major section(the southwest part)of the Yingxiu-Beichuan co-seismic rupture zone and the Guanxian-Anxian co-seismic rupture zone are corresponding with the exposed area of the Upper Triassic Xujiahe coal-bearing strata in the Longmen Shan region.The Upper Triassic Xujiahe coal seam and the Middle-Lower Triassic and Silurian,Cambrian shales in the Longmen Shan region are the flexible rock layers,which are easy to slide and form detachment surface or detritus within the fault zone.The co-seismic rupture zone produced by the May 12 Wenchuan Ms 8.0 great earthquake resulted from a B-type sliding along the flexible rock layers in the shallow crust level.
【Fund】: 中国地震局地震动力学国家重点实验室自主课题(LED2008A02);; 国家自然科学基金项目(40472090)资助
【CateGory Index】: P315.2
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6 TANG Yong1,2),QIN Jian-xiong1),LI Yan-hong2),ZHAO Jun2),LIANG Yan-tao2),LIU Yan3)1)Commercial College,CDUT,Chengdu,Sichuan 610059;2)College of Earth-science,CDUT,Chengdu,Sichuan 610059;3)School of Foreign Affairs,SCNU,Chengdu,Sichuan 610110;The Classification and Qualitative Evaluation of Wenchuan Earthquake Vestige Landscape for Tourism[J];Acta Geoscientica Sinica;2010-04
7 ZHANG Yong-jiu ZHANG Zhi-wei(Earthquake Administration of Sichuan Province,Chengdu 610041,China);THE FOCAL MECHANISMS AND CHARACTERISTIC OF STRESS FIELD IN ZIPINGPU AREA BEFORE WENCHUAN EARTHQUAKE[J];Seismology and Geology;2010-04
8 HU Xian-ming SHAO Yu-ping(Earthquake Administration of Sichuan Province,Chengdu 610041,China);CALCULATION METHOD OF MONITORING CAPABILITY OF RESERVOIR SEISMIC NETWORK——BASED ON G-R RELATIONSHIP[J];Seismology and Geology;2010-04
9 MA Wen-tao1) XU Chang-peng1,2) ZHANG Xin-dong3) XU Xi-wei1) LI Hai-ou1) YUAN Jing-li1) 1)National Geophysical Field Observatory at Lhasa,Institute of Geology,China Earthquake Administration,Beijing 100029,China 2)Earthquake Administration of Shandong Province,Jinan 250014,China 3)Handan Seismic Station of Earthquake Administration of Hebei Province,Handan 056001,China;STUDY ON THE RELATIONSHIP BETWEEN THE RESERVOIR-INDUCED SEISMICITY AT ZIPINGPU RESERVOIR AND THE M_S 8.0 WENCHUAN EARTHQUAKE[J];Seismology and Geology;2011-01
10 DANG Jia-xiang ZHOU Yong-sheng HAN Liang HE Chang-rong CHEN Jian-ye DANG Xin-zeng YANG Xiao-song(State Key Laboratory of Earthquake Dynamics,Institute of Geology,China Earthquake Administration,Beijing 100029,China);X-RAY DIFFRACTION ANALYSIS RESULT OF CO-SEISMIC FAULT GOUGE IN CARBON MUDSTONE AT OUTCROPS OF BAJIAOMIAO AND SHENXIGOU IN HONGKOU[J];Seismology and Geology;2012-01
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6 LIU Shu gen 1, ZHAO Xi kui 1, LUO Zhi li 1, XU Guo sheng 1, WANG Guo zhi 1, C.J.L.Wilson 2, Dennis Arne 3 (1.Chengdu University of Technology, China; 2.Melbourne University, Australia; 3.University of Ballarat, Australia);STUDY ON THE TECTONIC EVENTS IN THE SYSTEM OF THE LONGMEN MOUNTAIN-WEST SICHUAN FORELAND BASIN, CHINA[J];Journal of Chengdu University of Technology;2001-03
7 HUANG Zeguang1,2, JIA Cunshan2, XU Hongjie1(1.Dept.of Petroleum, Chengdu University of Technology, China;2.Wuxi Research Institute of Experimental Petroleum Geology, SINOPEC, China) ;CORRELATION OF THE STRUCTURAL DEFORMATION FEATURES BETWEEN KUCHE DEPRESSION IN TARIM BASIN AND WEST SICHUAN DEPRESSION IN SICHUAN BASIN[J];Journal of Chengdu University of Technology(Science & Technology Edition);2003-05
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