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《Journal of Geodesy and Geodynamics》 2006-03
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DEFORMATION FIELD AND TECTONIC STRESS FIELD CONSTRAINED BY GPS OBSERVATIONS IN NORTH CHINA

Liu Xia1,2,3),Fu Rongshan1,2),Yang Guohua3),Sun Dongping3), Dong Yunhong3) and Han Yueping3)1)School of Earth and Space Sciences, University of Science and Technology of China, Hefei 2300262)Key Laboratory of Crust-Mantle Materials and Environments, CAS,Hefei 2300263)First Crust Monitoring and Application Center, CEA, Tianjin 300180  
The 3D FEM model of North China was created, which had been incorporated with the data of tectonic, Quaternary active faults, topography, the thickness of crust and crust-uppermantle velocity structure. Having constrained by GPS observations as boundary condition, the deformation and tectonic stress fields were simulated. The calculation result show that the predicted surface velocity field is very consistent with the GPS observations. In these results, large NNE trending faults, such as Fenwei graben fault system, manifest itself of right-lateral slip, and NWW trending fault system, such as Zhangjiakou-Bohai fault system, left-lateral slip, which are in accordance with the results from field geological inspection. For the predicted stress field in the depth of 10-20 km below the earth surface, the direction of the principal compressive stress is NNE-EW, the principal tensile stress is about 3-8 times larger than the principal compressive stress. In the maximal shear stress field, there are three high gradient zones located in Shanxi region, the central North China plain and the coast region of East China, respectively,these zones correspond to main active earthquake zones in the studied region.
【Fund】: 国家自然科学基金(40574073)
【CateGory Index】: P315.725
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