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《Chinese Journal of Geophysics》 2006-03
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Deep geophysical probe and geodynamic study on the Qinghai-Tibet Plateau (1958—2004)

LU Zhan-Wu,GAO Rui,LI Qiu-Sheng,GUAN Ye,ZHANG Ji-Sheng,HE Ri-Zheng,HUANG Li-YanLithosphere Research Center,Institute of Geology,CAGS,Beijing 100037,China  
Chinese geophysicists carried on a series of geophysics research on the crust and upper mantle of Qinghai-Tibet plateau since 1958 and the total investigation length is about 45000km.In order to express the achievements in all aspects,the authors collect materials extensively,summarize the geophysical work on the crust and upper mantle of Qinghai-Tibet plateau,and draw a series of work degree figures according to different methods.This article gives a systematic account of the crustal structure,lateral heterogeneity of the upper mantle,resistivity of the lithosphere,uplifting mechanism of the Qinghai-Tibet plateau,geodynamic model and numerical simulations on lithosphere tectonic stress field.The available data shows that Moho is comparatively deep in this area.From south to north,Moho has different depths and features undulation beneath several main sutures.The results show that there is generally a discontinuous layer of low velocity and high conductivity in the crust of Tibetan plateau,which exists in 20±5km depth generally with a velocity of 5.6~5.8km/s,a low resistivity of 1~10Ω·m and a thickness of 5~10km.The low velocity layer and high conductivity layer are similar but not same in the depth and thickness.The natural earthquake research achievements show similar seismic anisotropy direction in every block on Qinghai-Tibet plateau,but there is obvious change at the boundary of blocks.Though there are different opinions regarding the uplifting history of Qinghai-Tibet plateau,it has been generally acknowledged that the plateau has undergone multi-phase uplift under multiple action mechanisms.On the basis of the results of comprehensive geophysical survey and interpretation and geological information,a geodynamic model was built to demonstrate the deformation mode of the plateau lithosphere.
【Fund】: 国家自然科学基金重点项目(40334035);; 中国国土资源部“中国岩石圈三维结构数据库”项目(200010101)联合资助
【CateGory Index】: P541
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