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《Chinese Journal of Geology(Scientia Geologica Sinica)》 2008-04
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Active modes and mechanisms of the Paleozoic faultings in western Tarim

Li Yuejun1 Wu Genyao1 Meng Qinglong1Shi Jun2 Feng Xiaojun2 Zheng Min3(1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029;2.Tarim Oilfield Branch Company,China National Petroleum Corp.,Korla,Xinjiang 841000;3.Lanzhou Oil-Gas Resource Centre,Institute of Geology and Geophysics,Chiinese Academy of Sciences,Lanzhou 730000)  
Based on systematic interpretation of seismic profiles and a comparative study to central area of the Tarim Basin,the active modes and mechanisms of the Paleozoic faultings in western Tarim were explored in the paper.The NE-striking Madong(Badongnan)fault zone,as a part of southeastern boundary of the Bachu Fault-Uplift,was a superficial décollement fold-and-thrust belt,and expanded southeastwards.The piggy-back thrusting occurred in the end of Ordovician.The NW-striking Badong fracture(or the No.2 Tumxuk fracture),the eastern boundary of the Bachu Fault-Uplift,was a basement-involved thrust,with the thrusting occurring in the ends of Ordovician and Middle Permian respectively.The Baxi and South of Well Tacan 2 fractures in north part of the Markit Slope were Hercynian normal faults.The Paleozoic development of the Tarim paleo-plate was constrained by the neighbouring orogenic evolution.The thrusting of nearly W-E and NE-striking fractures in early Caledonian,related to subduction of the West Kunlun ocean,might inherit the basement structures.The NW-striking fractures in central Tarim was neogenic in Late Cambrian,in which two episodes of Caledonian deformation could be recognized:the early thrusting in the end of Ordovician and late thrusting and strike-slipping during Late Silurian to Middle Devonian.The later deformation should be resulted from the activation of the Paleo-Altun shearing orogen,so as to obviously become weeker westwards.Some NW-striking fractures in west Tarim,for example,the Kangxi fracture,attached to the Tazhong(central Tarim)NW-striking fracture system.The NE-striking Madong fault zone was a transfer fault between the Tumxuk fault zone(thrusting towards the north to east)and the Wells Tazhong 8-1 and Tazhong 5 fault zone(thrusting towards the south to east).
【Fund】: 国家“973”项目(编号:2006CB202301);; 中国科学院知识创新工程重要方向项目(编号:KZCX3-SW-147);; 国家“十五”重点科技攻关项目(编号:2004BA16A02)的部分成果
【CateGory Index】: P618.13
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