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《Chinese Journal of Geophysics》 2013-01
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Numerical simulation on the special gravity fields and dynamic response in Longmenshan orogenic belt and adjacent area

YANG Hui1,2,TENG Ji-Wen1*,WANG Qian-Shen1,PI Jiao-Long1 1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2 State Key Laboratory of Geodesy and Earth′s Dynamics,Institute of Geodesy and Geophysics,CAS,Wuhan 430077,China  
The Longmenshan orogenic belt is in a very non-isostatic state,which means its crust is in an unstable state.In this paper,2-D Finite Element Method is used with viscoelastic model to study the geodynamical mechanism of gravitational isostasy through the profile across the Songpan-Garze block,Longmenshan faults and Sichuan basin.The results show that:(1) The motion mode of deep materials is much changed by the isostatic adjustment.The interaction effects of the India plate collision and the gravity potential energy cause the dynamics of the sub-vertical downward asthenospheric flow at the bottom of the Longmenshan lithosphere,and lead to the exceptionally steep topography at the eastern Tibetan margin as a result of gravitational buoyancy.(2) The distribution of strain-energy,the rheological structure and other results are calculated numerically,which show that the sections with high risk factors coincide with the areas of the Wenchuan earthquake.The different geophysical structures,as well as the different rheological model on both east and west side of Longmenshan faults zone played important roles in the seismogenic mechanism of the Wenchuan earthquake.(3) We suggest that crustal shortening together with isostatic adjustment,including the rapid erosion-related unloading,is a key component of the geodynamic processes on the eastern Tibetan Plateau margin.
【Fund】: 国家自然科学基金(41104059);; 中国科学院动力大地测量学重点实验室开放基金(L09-08);; 地下信息探测技术与仪器教育部重点实验室(中国地质大学 北京)开放课题项目(GDL0906)联合资助
【CateGory Index】: P312
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