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《Seismology and Geology》 2003-04
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CONTEMPORARY CRUSTAL DEFORMATION AND ACTIVE TECTONIC BLOCK MODEL OF THE SICHUAN-YUNNAN REGION,CHINA

Lü Jiang ning 1) SHEN Zheng kang 2) WANG Min 3) 1) Department of Geophysics, School of Earth and Space Science, Peking University, Beijing 100871, China 2) Institute of Geology, China Seismological Bureau, Beijing 100029, China 3) Center for Earthquake Analysis and Prediction, China Seismological Bureau, Beijing 100036, China  
We derive horizontal velocity field of the Sichuan Yunnan region by analyzing GPS data collected from the Crustal Movement Observation Network of China between 1998 and 2001. Our result shows that the region is composed of 4 tectonic terrains: the Chuan Dian block, the Longmen Shan region, the Red River shear zone, and the Ruili Ximeng region. The Chuan Dian block is further decomposed into 3 sub blocks: the Dianzhong block, Yajiang block and Zhongdian block. The Longmen Shan region is decomposed into the Minshan block and the Aba region. Viewed relative to the Eurasian plate, the Dianzhong block, Yajiang block and Zhongdian block are rotating clockwise at 0.37°±0.16°/Ma, 0.84°±0.39°/Ma and 0.90°±0.39°/Ma, respectively, resulting in active faulting between the sub blocks: ~3 mm/yr north south shortening across the Muliarcuate Fault, ~4 mm/a east west extension across the Lijiang Fault, and ~6mm/a east west extension across the Litang Fault. About 8~10mm/a left lateral strike slip is detected across the Xianshuihe Fault, and 5~6mm/a left lateral strike slip across the Anninghe Zemuhe Xiaojiang Fault. No obvious crustal shortening is observed across the Longmen Shan Fault. About 150km northwest of the Longmen Shan Fault lies a velocity gradient zone with a 4~5mm/a right slip across. The Minshan block and the Aba region bounded by the gradient zone rotate counterclockwise at 0 13°±0 08°/Ma and 0 53°±0 19°/Ma relative to the Eurasian plate, respectively. Our results are consistent with a model attributing the crustal deformation of the Chuan Dian block in the Sichuan Yunnan region to be driven mainly by the eastward extrusion and gravitational collapse of the Tibetan Plateau. Being resisted by the relatively stable south China block to the east, the Chuan Dian block turns from eastward to southward motion along the Xianshuihe Xiaojiang Fault, resulting in a cluster of clockwise rotations of its internal sub blocks.
【Fund】: 国家重点基础研究发展规划项目 (G19980 4 0 70 3)资助
【CateGory Index】: P542
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