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《Crustal Deformation and Earthquake》 2000-03
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NUMERICAL SIMULATION OF THE EVOLUTION OF THE DEFORMATION AND STRESS PATTERNS IN THE EAST ASIA CONTINENT

Fu Rongshan 1,2) , Huang Jianhua 1,2) , Chang Xiaohua 3) and Cao Kangzhen 1,2) 1)Department of Earth and Space Sciences,University of Science and Technology of China, Hefei, 230026 2)Advanced Research Center for Geoscience and Astronomy,third  
A numerical simulation is employed to study the evolution of the Tibet Plateau's uplift and the deformations and the stress patterns in the region of EastAsia continent after the collision between Indian and Eurasian plates.In this model the EastAsia continent is limited in a trapezoid geological frame and the continental lithosphere is regard as a continuum thin plate with a power law rheology.It overlies on a relative soft uper mantle.The movement of the Indian plate at the rate of 5 cm/a is assumed to be the main driving force driving the Tibet Plateau's uplift and the lithosphere deformation of the EastAsia continent.The numerical simulation shows that the predicted rates of the horizontal deformations of the EastAsia continent can fit to the results of the GPS observation very well.Meantime,the predicted stress patterns can fit the observation data set too.It implicates that the collision and compression between India and Eurasia plates is the main driving force of the horizontal deformations and the stress field of the EastAsia continent.It also shows that the patterns of the continental deformation are controlled by many factors such as the dynamical parameters of the lithosphere and the boundary conditions as well.
【CateGory Index】: P55
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