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《EARTH SCIENCE FRONTIERS》 1999-04
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STRUCTURAL PATTERN AND TECTONIC EVOLUTION OF NNE TRENDING STRIKE SLIP OROGENIC BELT IN THE BORDER REGION OF HUNAN AND JIANGXI PROVINCES

Fu Zhaoren Li Zijin(China University of Geosciences,Beijing,100083)Zheng Dayu(China National Nuclear Corporation,Beijing,100013)  
According to the principles and methods of structural analysis by professor Ma Xingyuan, the structural pattern and tectonic evolution of the NNE trending strike slip basin rang structure in the border region of Hu'nan and Jiangxi Provinces are discussed.The overpass superposed relationship between the pre Mesozoic EW trending paleo Tethyan tectonic system and the Mesozoic Cenozoic NNE trending marginal Pacific tectonic system as well as the tectonic background are verified.In this paper, a transform orogenic model of continental crust underthrust convergent strike slip in South China landmass is establised, and the conception of Neocathaysian metamorphic core complex is proposed.At the same time its fundamental features and forming mechanism are also discussed.This paper emphasizes that the NNE trending strike slip fault in the border region of Hu'nan and Jiangxi Provinces is a main part of the southern section of the Tan Lu fault belt.On the earth's surface,it shows as an echelon lozenge network system and was formed by the intersection of the NE30° trending synthetic strike slip fault(P) and the NW320° trending antithetic strike slip fault(R′), that so constituted the basic structural pattern.Most granites of the continental crust underthrust group(γ 1 5)and the convergent strike slip group(γ 2 5)were formed by shear remelting. The echelon style arranged semi graben basins and the Neocathaysian metamorphic core complexes are controlled by strike slip and extension deformation field.The border region had experienced two processes of tectonic transformation and two strike slip orogenies processes with different movement nature and tendency after later Triassic epoch(T 3).These were shown as the transformation from continental crust underthrust to strike slip(210 Ma)and convergent strike slip orogeny in Jurassic period(J),and also as the transformation from the convergent to the divergent strike slip(K 1)and the divergent strike slip orogeny in Cretaceous Palaeogene period(K—E).Each of them had played a significant role in diagenesis and mineralization.
【Fund】: 国家自然科学基金项目;核工业中南地质局项目
【CateGory Index】: P542
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9 Xu Jun-Yuan(Research Institute of Geology, Anhui Province);APPROACH TO THE MATHEMATICAL EXPRESSIONS OF THE FUNCTIONS OF SHEAR STRAIN γ(x) AND DISTORTION DISTANCE s(x) ACROSS DUCTILE SHEAR ZONES[J];Seismology and Geology;1987-01
10 Tong Weixing(Department of Geology, Hefei Polytcchnical University, Hefei);RESEARCH ON DEFORMATION OF THE FAULT TERMINATION IN SOUTHERN SEGMENT OF THE TANCHENG-LUJIANG FAULT ZONE, THE BORDER OF ANHUI AND HUBEI PROVINCES[J];Chinese Journal of Geology;1987-03
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