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《Chinese Journal of Geophysics》 2006-02
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Dynamic simulation of lithospheric evolution from the modern China mainland and its surrounding areas

ZHENG Yong 1,2, FU Rong-Shan1, XIONG Xiong31 School of Earth Space Science, University of Science and Technology of China, Hefei 230026, China2 Institute of Geophysics, China Earthquake Administration, Beijing 100081, China3 Wuhan Institute of Geodesy and Geophysics, Wuhan 430077, China  
Recent 0.2Ma evolution of lithosphere in the China mainland is modeled using finite element analysis.The effects of collision between Eurasia and Indian Plates on the strain and stress field in the China mainland are studied. Combining with GPS surveys, seismological data and geological analysis, we try to probe into the basic patterns of strain and stress field in this area on the time scales of several million years, 0.1 million years and tens of years. The results show that the India-Eurasia collision and the stress environment caused by the continuous northward extrusion of the Indian Plate play a key role in controlling the tectonic movement and lithospheric evolution of the Tibetan Plateau and its surrounding areas, while in the regions far away from the Tibetan Plateau, it becomes weak. Faults and gravity potential produce significant effects on the eastern and the western parts of the Tibetan Plateau and Tarim Basin. In the Tibetan Plateau, these effects increase the rate of lateral deformation; in the southern parts of Tibet, they create an extensional stress field, while in the Tarim Basin, they make it dextrorotate. The calculated horizontal velocities are well consistent with GPS surveys. However, in vertical dimension, quite large differences are observed in some areas, which means modern uplifting of the Qinghai_Tibetan Plateau depends not only on the Indian-Eurasian collision, but also on other kinds of mechanisms, such as mantle convections, isostatic effects and all kinds of erosions. The calculated stress field is consistent with the observed data. The Indo-Asian collision has mainly controlled the principle tensional stress field in the western part of China, but other kinds of mechanisms, such as gravity and mantle convections, have a very important impact on the eastern Tibetan Plateau. The Indo-Asian collision controls the seismicity of the western part of China, but except North China, where the seismicity is very active while the calculated stress level is very low. This puzzle probably means that other forces have made the North China block reactive.
【Fund】: 中国科学院创新项目(KZCX3-SW-131);; 国家自然科学基金项目(40274033 40274037)资助.
【CateGory Index】: P313
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4 QIN Si-qing,XUE Lei,WANG Yuan-yuan,HUANG Xin,PAN Xiao-hua (Key Laboratory of Engineering Geomechanics,Institute of Geology and Geophysics, Chinese Academy of Sciences,Beijing 100029,China);Further verifications on the brittle failure theory of multiple locked patches along a seismogenic fault system and discussions on some science issues[A];[C];2011
5 CHEN Jie,WEI Cheng-long,LUO Wen-zao (Guangzhou Marine Geological Survey,Guangzhou 510075);Convoying for Ocean Geophysical Exploration[A];[C];2009
6 Yong Zheng Zujun Xie Rongjiang Wang Sidao Ni Xiong Xiong Can Ge GeoForschungsZentrum Potsdam(GFZ),Potsdam,Germany;;Effects of crustal variation on the focal mechanism inversion and relocation of the Wenchuan aftershocks[A];[C];2009
7 Zujun Xie Yong Zheng;Focal mechanisms of the southern aftershock swarm of Wenchuan Ms8.0 earthquakeand the seismotectonic implications[A];[C];2009
8 Chen Lianwang Zhan Zimin Ye Jiyang Li Yujiang Li Yan;Numerical modeling on influence of giant strike slip fault system to tectonic deformation pattern in Tibet plateau[A];[C];2011
9 Lijun Yan 1 , Jiahong Wen 2 , Jianping Yan 2 , Rui Liu 2 , Ke Chen 2 1 Department of Computer Center, Shanghai Normal University, Shanghai 200234,China 2 Department of Geography, Shanghai Normal University, Shanghai 200234, China;Comparing and Analyzing of Disaster Databases from Domestic and Abroad[A];[C];2012
10 Long Su~(a,b,*),Jianjing Zheng~a,Guojun Chen~a,Gongcheng Zhang~c,Jianming Guo~a,Yongchang Xu~a a Key Laboratory of Petroleum Resources Research,Institute of Geology and Geophysics,Chinese Academy of Sciences,Lanzhou,Gansu 730000,PR China b Graduate University of the Chinese Academy of Sciences,Beijing 100039,PR China c Research Institute of China National Offshore Oil Corporation,Beijing 100027,PR China;The upper limit of maturity of natural gas generation and its implication for the Yacheng formation in the Qiongdongnan Basin,China[A];[C];2013
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