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《Geotectonica Et Metallogenia》 2009-01
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The Cenozoic Fault System of Southeastern Tarim Basin

YANG Shufeng1,2,CHEN Lifeng1,2,XIAO Zhongyao3,LUO Juncheng3,4,CHEN Hanlin1,2,WANG Buqing3,CHENG Xiaogan1,2 and LIAO Lin1,2(1.Department of Earth Sciences,Zhejiang University,Hangzhou 310027,Zhejiang,China;2.MOE Structural Research Center of Oil and Gas Bearing Basin,Hangzhou 310027,Zhejiang,China;3.Petroleum Exploration and Development of Tarim Oilfield Company,PetroChina,Korla 841000,Xinjiang,China;4.College of Earth and Planetary Science,Peking University,Beijing 100871,China)  
Combined with the field geologic investigation,and the detailed interpretation of seismic,MT and other geophysical information,the fault system has been constructed in the southeastern Tarim basin.The cenozoic fault system of southeastern Tarim basin can be divided into three systems:the Altun fault system,Che'erchen fault system and the West Kunlun fault system.The Altun fault system is dominated by NW trending thrust which is accompanied by strike-slip.The Che'erchen fault system was composed of a series of secondary fault and thrust faults,which characterizes the northwestward thrust and the sinistral strike-slip.The West Kunlun fault system mainly consists of thrust faults which thrust from south to north.Near the intersection between the Altyn Mountain and the west Kunlun fault system,the later was curved by the impact of the former sinistral strike-slip.
【Fund】: 《塔东南坳陷-塔南隆起构造地质特征研究》项目(编号:041006060051)资助
【CateGory Index】: P542
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