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《Journal of Mineralogy and Petrology》 2006-04
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GEOMORPHIC AND SEDIMENTARY EVIDENCE FOR REVERSION OF STRIKE-SLIP DIRECTION IN LONGMEN SHAN FAULT ZONE

LI Yong~1,ZHOU Rong-jun~2,A L Densmore~3,M A Ellis~4 1.National Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology,Chengdu 610059,China; 2.Institute of Earthquake Engineering,Seismological Bureau of Sichuan Province,Chengdu 610041,China; 3.Institute of Geology,Department of Earth Sciences,ETH Zentrum, CH-8092 Zürich,Switzerland; 4.Center for Earthquake Research and Information,University of Memphis, 3890 Central Avenue,Memphis,TN 38152,USA  
Based on the evidence of migration of the depocentre and fan in the foreland basin,the active tectonics,geomorphy and paleomagnetism from Mesozoic to early Cenozoic and later Cenozoic,the direction of strike-slip faulting has been reversed from sinistral strike-slip in Mesozoic and early Cenozoic to dextral strike-slip in the later Cenozoic.According to stratigraphy and paleomagnetism,the reversion of the strike-slipping direction in Longmen Shan fault zone happened during 43 Ma to 3.6 Ma.It was considered that the dextral strike-slip in the later Cenozoic is due to the effect of post-India-Eurasian collision,and the sinistral strike-slip in Mesozoic and early Cenozoic is due to the effect of shorting of Songpan-Ganzi Fold Belt driven by accretion of the Cimmerian continents and the India/Eurasia collision.
【Fund】: 国家自然科学基金项目(编号49803013 40372084);; 高等学校博士学科点专项科研基金项目(编号20050616004);; 四川省重点学科建设项目(编号SZD0408);; 中国石油化工公司重大前瞻性研究项目(G0800-06-25-282)
【CateGory Index】: P542
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