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《Crustal Deformation and Earthquake》 2004-01
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HORIZONTAL CRUSTAL MOVEMENT OF TIBETAN PLATEAU FROM GPS MEASUREMENTS

Gan Weijun1), Shen Zhengkang1,2)\ Zhang Peizhen1),Ren Jingwei1),Wan Yongge3,1) and Zhou Demin\+\{1)\} 1)Crustal Movement Research Center,Institute of Geology,CEA, Beijing\ 100029 2)Department of Earth and Space Sciences,University of California,Los Angeles,CA 90095 1567,USA 3)College of Disaster prevention Technology,CEA,Beijing\ 101601  
Using the measurements of over 580 GPS stations located around the Tibetan plateau,we derive a spatially dense horizontal velocity field of the region.In order to better visualize the differential motion among stations within the plateau,we transform the velocity field into a “Tibetan plateau fixed reference frame”.The velocity field shows that:①For the southeast region of the plateau bounded by the Mani Yushu Xianshuihe fault the most remarkable horizontal movement is a clock wise“flow zone”around the Eastern Himalayan Syntaxis.The velocity field of the “flow zone”has a fan like shape in the southeastern corner of the plateau,implying that the “flow zone”could be attributed to the escape of a high plastic upper crust material driven by the lateral compression and gravitational buoyancy.②The northeastern region of the plateau located between the Mani Yushu Xianshuihe fault and the Haiyuan fault appears to be a uniform left lateral shear zone overall.However,such a shear deformation is not significant in the Longmenshan area along the east margin of the Tibetan plateau.The Sichuan basin and its northern neighborhood region do not accommodate significant shortening either.Therefore,the northeastern region of the Tibetan plateau does not show significant eastward motion with respect to the rest part of the plateau.③The most significant velocity gradients within the plateau exist across the Altyn Tagh,Haiyuan,and Mani Yushu Xianshuihe faults,reflecting extensive activities there.Because of the “dragging”associated with the eastward escape of the plastic flow zone between the Mani Yushu Xianshuihe fault and the Karakunlun Jiali fault,the north and south regions of the flow zone display left and right lateral shear respectively.
【Fund】: 国家自然科学基金项目 (4 0 2 740 3 4);; 科技部基础研究重大项目前期研究专项(2 0 01CCB0 110 0 )项目
【CateGory Index】: P228.4
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