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《Earth Science Frontiers》 2003-S1
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DEFORMATION RESPONSES TO EASTWARDS ESCAPING OF THE QINGHAI-TIBET PLATEAU AND TECTONICS OF THE SOUTH-NORTH SEISMIC ZONES IN CHINA

ZHANG Jia-sheng 1, LI Yan 2, HAN Zhu-jun 1 (1.Institute of Geology, China Seismological Bureau, Beijing 100029, China; 2.Exploration and Production Research Institute, SINOPEC, Beijing 100083, China)  
Various deformation responses to the eastwards escaping of the Qinghai-Xizang (Tibet) Plateau occurred in the adjacent blocks of Sichuan, Ordos, Chuandian and Dianxi. According to the tectonic interpretation of aeromagnetic anomalies in the regions of Sichuan and Ordos basins, and field investigation carried out in west Yunnan Province, the Ordos block was contorted in left lateral sense along a series of E-W trending strike slip faults, which occurred in the high-grade metamorphic basement following previous thrusts; while the metamorphic folded basement under Sichuan basin had shortened parallel to Longmenshan thrusts. The Dianxi and Chuandian block moved in left lateral sense along Jinshajiang—Honghe fault earlier (around 20 Ma) and along Xianshuihe—Xiaojiang fault later (about 5 Ma), respectively. The neotectonic events that occurred in Dianxi, Chuandian, Sichuan and Ordos regions represent the marginal and long distance effects resulting from the syn-tectonic extension of the Qinghai-Xizang Plateau, which overprinted and reworked all previous structures in the blocks. It seems that the deformation developed from south to north and from cover to basement progressively, and weakened from west to east. The seismicity caused by recent deformation in multi-levels and multi-stages at the east edge of Qinghai-Xizang Plateau makes up the South-North Seismic Zone.
【Fund】: 国家自然科学基金资助项目 (4 0 172 0 77) ;; 国家重点基础研究发展规划项目 (2 0 0 1CB7110 0 2 )
【CateGory Index】: P315.2
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