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《Geotectonica Et Metallogenia》 2008-01
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CHARACTERISTICS OF THE TASHUIHE DUCTILE SHEAR ZONE,EASTERN TIANSHAN,XINJIANG

MA Huadong1,2,HE Weidong3,TU Qijun4,CHEN Jing5,CAO Fugen3 and REN Yan3(1.Guangzhou Institute of Geochemistry Chinese Academy of Sciences,Guangzhou 510640,Guangdong,China;2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China;3.No.1 Party of BGMR,Urumqi 830011,Xinjiang,China;4.Xinjiang Geological Survey,Urumqi 830000,Xinjiang,China;5.Institute of Environmental Protection Monitoring and Inspection of BOLR,Urumqi 830011,Xinjiang,China)  
The Tashuihe ductile shear zone is located in southern Haerlike Mountain to the south of Tashuihe fault.It experienced a severe deformation characterized by the macrostructure and subminiature pictures,demonstrating multidirections and other typical features of shearing.The deformation was developed over two time periods:the late Ordovician during which the reverse nappe and right-lateral shearing was formed by the northward compressive stress field,and the late Carboniferous while the uplifting decollement and left-lateral strike-slip was formed by shear stresses caused by the granite intrusions.An overall displacement for each of the two time periods is,respectively,2.2 km and 2.46 km,corresponding to a differential paleo-stress of 82 Mpa and 89 Mpa.
【Fund】: 新疆伊吾县伊吾河上游一带1∶5万区域地质矿产调查(项目编号:XJQDW2003-07)
【CateGory Index】: P542
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