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《Journal of Changchun University of Science and Technology》 2001-03
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STUDY ON TUMUXIUKE FAULT BELT IN TARIM BASIN

LIU Zhi_hong 1,LIN Dong_cheng 2,WANG Wen_ge 2, ZHANG Li_guo 2,GAO Jun_yi 2,REN Lin_wei 2,LIU An_ying 2 (1.College of Earth Sciences, Jilin University, Changchun 130061,China; 2. Research Institute of Exploration and Development, Daqing Oil fi  
The research area is situated in the western part of Tarim basin. It can be divided into Bachu block uplift and Awati depression by Tumuxiuke fault belt. The study of geometry, kinematics and geodynamics of Tumuxiuke fault belt show that the Tumuxiuke fault belt is a dextral reversed strike-slip fault which formed along the axial surfaces of the fault band fold or fault propagation fold. It destructed the early structures and controlled the formation and development of Bachu block uplift and Awati depression. Tumuxiuke fault belt was formed from Tertiary, and caused by the remote effect of India-Tibet collision. Up to now it has been activity.
【Fund】: 大庆油田有限责任公司研究项目“塔里木盆地大庆区块断层封闭性研究”资助
【CateGory Index】: P542.3
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