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《Journal of Jiling University (Earth Science Edition)》 2005-05
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Space-time Distribution Features,Migration Regularities and Genetic Types of Regional Fault System of Meso-Cenozoic in the Central Section of Epicontinent of the East China

SUN Xiao-meng~(1),WANG Pu-jun~(1),HAO Fu-jiang~(2),BAO Ya-fan~(3),MA Xu~1,HAN Guo-qing~1(1.College of Earth Sciences,Jilin University,Changchun130026,China;2.College of Applied Technology,Jilin University,Changchun130022,China;3.Third Geological Survey,Jilin Province,Siping136000,China)  
Deep and large faults developed very well in the central section of epicontinent of the East China.Based on the space-time distribution of the faults,four fault systems are divided,namely,Yan-(shan) orogenic belt fault system,Qinling-Dabie-Sulu orogenic belt fault system,Tanlu fault system and East China Sea shelf basin-Okinawa trough fault system.The four fault systems have different migration regularities of the faults.The faults of Indosinian epoch-Yanshan epoch of Yanshan orogenic belt have deflective migration regularity from EW direction to NE direction to NNE direction from the early to the late periods.The strength of thrust-nappe of the Qinling-Dabie orogenic belt fault system shows a(tendency) of being strong in the south and in the east,weak in the north and in the west and of faulting in the east and folding in the west in Indosinian-early Yanshan epochs.Meanwhile,the faults have the feature of diachronous migration evolution from the east to the west from the early to the late periods.On the contrary,the last Yanshanianearly Himalayaian epochs show the tectonic feature of being strong in the north and in the west,weak in the south and in the east.The activity and basin-controlling function of the Talu fault system are characterized by the migration from south to north from early to late periods.The formation time of the East China Sea shelf basin-Okinawa trough fault system become apparently younger from west to east.The four fault systems and their structural migration are the products of different geodynamic backgrounds: collision of plates,intracontinental subduction,intracontinental orogency,strike-slip,plate subduction and retreat.
【Fund】: 国家自然科学基金项目(40272043);; 中国石油天然气集团总公司“九五”科技工程项目(970206-01);; 中国石油化工股份有限公司“十五”科技开发项目(P00002)
【CateGory Index】: P542.3
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7 Shan Wenlang Fu Zhaoren (Wuhan College of Geology, Wuhan 430074);A PRELIMINARY ANALYSIS OF THE HORIZONTAL LAMINAR SHEAR-FLOW STRUCTURE IN THE WEST-HILL,BEIJING[J];;1987-02
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9 Jin Shuyan Jiao Shuqiang(Faculty of Earth Sciences, China University of Geosciences, Wuhan430074);FABRIC MEASUREMENTS OF OMPHACITE FROM ULTRAHIGH PRESSURE ECLOGITE AND ITS RHEOLOGICAL SIGNIFICANCE[J];;1998-01
10 Zhong Zengqiu Suo Shutian You Zhendong (Faculty of Earth Sciences, China University of Geosciences, Wuhan430074);EXTENSIONAL TECTONIC FRAMEWORK OF POST HIGH AND ULTRAHIGH PRESSURE METAMORPHISM IN DABIESHAN, CHINA[J];;1998-03
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