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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2008-04
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A preliminary study on the 3-D crust structure for the Longmen lithosphere and the genesis of the huge Wenchuan earthquake,Sichuan,China

CAI Xue-lin1,CAO Jia-min2,ZHU Jie-shou2,CHENG Xian-qiong21.College of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China;2.College of Information Engineering,Chengdu University of Technology,Chengdu 610059,China  
Based on a structural analysis of many seismic sounding profiles,there are two fault systems in Longmen collisional orogenic belt,Sichuan,China.They are both different obviously and correlative closely.One is shallow fault system composed mainly of brittle shear zones in surface crust,and the other is deep fault system composed mainly of crust-mantle ductile shear zones cutting Moho discontinuity.Based on the result of researching geological structure and seismic sounding profiles,the authors give a lithospheric crustal structure model of the Longmen orogenic belt and its adjacent areas besides generalizing the feature and relationship of the two fault systems.The authors think that the lithospheric crust-mantle ductile shear zone is one of the seismogenic structures and put forward the geodynamic model of a major earthquake.
【Fund】: 国家自然科学基金重点资助项目(49734150 40234047);; 国家自然科学基金资助项目(40474032);; 国土资源部专项计划资助项目(20001010206);; 成都理工大学青年基金资助项目(2006QJ12)
【CateGory Index】: P315.2
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