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《Acta Geologica Sichuan》 2011-04
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Structural Styles and Their Deformation Mechanism in the Middle Zone of the South Dabashan Foreland Thrust Fault Belt

DU Kun1 ZENG Qiang2(1-Geophysical Exploration Team,SBGEEMR,Chengdu 610072;2-Regional Geological Surveying Team,BGEEMRSP,Chengdu 610213)  
Three structural zones such as root zone,middle zone and frontal zone were developed in the South Dabashan foreland thrust fault belt.Field study of the middle zone in Muguakou-Mingyue and Chengkou-Longtian areas indicates that the imbricate fault zone have experienced seven movements,including three propagation thrust movements in NE-SW direction,one right-lateral shear movement in SE-NW direction,one thrust-right-lateral shear movement in E-W direction,one left-lateral shear movement and one normal-fault movement in NE-SW direction.In combination with previous geochronologic data,this paper makes an approach to the deformation mechanism of the South Dabashan foreland thrust fault belt which is of importance to the tectonic framework and ore-formation in the Qinling orogenic belt
【CateGory Index】: P542
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