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《Geology of Anhui》 2010-01
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FEATURES, ATTRIBUTES AND RESEARCH IMPLICATIONS OF TRANSFER STRUCTURE KNOTS ALONG THE MIDDLE-LOWER YANGTZE RIVER REACHES

SONG Chuanzhong1,HUANG Wencheng1,LIN Shoufa1,2,REN Shenglian1,LI Jiahao1,TU Wenchuan1(School of Resources and Environmental Engineering,Hefei University of Technology,Hefei 230009;2.Department of Earth Sciences,University of Waterloo,Ont.,Canada N2L 3G1)  
The transfer structure knots along the middle-lower Yangtze River reaches are the focal points where the Tethys tectonic mechanism meets,links up and transforms with the Pacific tectonic mechanism,substantially including the Dabie Orogen,Tan-Lu Fault and Middle-lower Yangtze metallogenic belts,referred to as three major well-known tectonic units,which are typical of deep-seated process and surface response of eastern China mid-Cenozoic continental dynamics.It will greatly favour new breakthrough in continental dynamic theory and guide deep-seated ore prospecting in "second metallogenic space" to combine continental orogen,large faults and mining camp,aim at intra-plate deformation,kinetics and dynamics,build up systematic research frame for continental dynamics in the area,study the delicate transformation process between two major tectonic mechanisms,and analyze the deep process and shallow effect of intra-continental tectonic evolution and dynamics..
【Fund】: 国家自然科学基金项目(批准号:40372097 40772131);; 安徽省公益性地质研究项目;; 中石化基础研究项目共同资助
【CateGory Index】: P541
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