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《Earth Science Frontiers》 2003-03
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COUPLING BETWEEN STRIKE-SLIP FAULTS AND BASINS:THE EVIDENCE FOR CENOZOIC EASTWARD EXTRUSION OF THE WEST QINLING-SONGGAN BLOCK

JIANG Xiao-wei~1,WANG Jiang-hai~(1,2),ZHANG Hui-hua~1(1.Guangzhou Institute of Geochemistry, Chinese Academy of Science, Guangzhou 510640, China;2.College of Life Sciences, Sun Yat-sen University, Guangzhou 510275, China)  
The Cenozoic eastward extrusion of the West Qinling-Songgan(Songpan-Garze) block is a major response in strain pattern, in NE Tibet induced by the Indion-Eurasian Continental collision. This extrusion belt is a northern branch of the strike-slip extrusion zone of the east Tibet. This branch, together with the southern branch, i.e., the Indochina extrusion belt may mutually regulated and absorbed the strain in east Tibet from the continental collision. The temporal-spatial coupling between the Minxian-Dangchang strike-slip fault with Cenozoic basins in West Qinling indicates that the existence of the eastward strike-slip and extrusion processes, which may provide a ruler for quantitative measuring of the extent of extrusion. The quantities of strike-slip displacement of the Minxian-Dangchang fault are 36 km in Paleogene and 76 km in Neogene respectively, and their corresponding strike-slip rates are 0.086 mm/a and 0.37 mm/a. This result suggests that the West Qinling-Songgan block was eastwards extruded at least up to 112 km in the Cenozoic. The Cenozoic mantle-derived magmatism in West Qinling was induced by the coupling among the ceasing of the block's rotation, the deformation of the fault planes and the accelerated strike-slip in the overall extrusion setting, and was also a recorder that records the status of the material and time of the strike-slip. Our studies suggest that the Minxian-Dangchang strike-slip fault affected the basal part of the lithosphere, recording the time of the dynamic change in NE Tibet from block rotation to rapid strike-slipping , i.e. the eastward extrusion of the West Qinling-Songgan block took place in the period of 21.1~25.4 Ma.
【Fund】: 国家重点基础研究发展规划项目 (G19980 40 80 7) ;; 广东省自然科学基金项目 (990 5 3 1) ;; 中国科学院知识创新项目(KZCX2 SW 117) ;; 国家自然科学基金资助项目 (4 9972 0 2 6) ;; 美国自然科学基金资助项目
【CateGory Index】: P544.4
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7 Liu Hefu (Department of Energy Resources Geology, China University of Geosciences, Beijing 100083)Liang Huishe (Hebei College of Geology, Shijiazhuang 050031)Cai Liguo (Department of Energy Resources Geology, China University of Geosciences, Beijing 100083)Xia Yiping (Third Geophysical Survey Division, BGP, CNCP, Zhengding 050800)Liu Liqun (Institute of Petroleum Geology, MGMR, Beijing 100083);Evolution and Structural Style of Tianshan and Adjacent Basins, Northwestern China[J];;1994-06
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9 Li Tingdong(The Chinese Academy of Geological Sciences);The Uplifting Process and Mechanism of the Qinhai-Tibet Plateau[J];;1995-01
10 Xu Zhiqin; Yang Jingsui; Jiang Mei; Li Haibing(Institute of Geology, Chinese Academy of Geological Sciences, Beijing, 100037);CONTINENTAL SUBDUCTION AND UPLIFTING OF THE OROGENIC BELTS AT THE MARGIN OF THE QINGHAI-TIBET PLATEAU[J];EARTH SCIENCE FRONTIERS;1999-03
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