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《Earth Science(Journal of China University of Geosciences)》 2007-04
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The Electrical Structure and Fault Feature of Crust and Mantle of Western Tibet Plateau:Based on Results of Magnetotelluric Survey along Profile Zhada-Quanshuihu

JIN Sheng1,2, YE Gao-feng1,2,WEI Wen-bo1,2,DENG Ming1,2,JING Jian-en1,21. State Key Laboratory of Geological Processes and Mineral Resources; Geo-detection Laboratory of the Ministry of Education, Beijing 100083, China 2. School of Geophysics and Information Technology, China University of Geosciences, Beijing 100083, China  
The research of magnetotelluric (MT) on the profile along Zhada-Quanshuihu on the west of the Tibetan plateau shows that the area is divided into three structural parts by Yalung Tsangpo suture and Bangong-Nujiang suture. From south to north they are Himalaya terrane, Gandese terrane and Qiangtang terrane. The area is widely distributed with high conductive layers, with fluctuating tops. The high conductive layer of Gandese terrane is deeper while that of Qiangtang terrane and Himalaya terrane is shallower. And the deepest high conductive layer is along the south of Bangong-Nujiang suture. The top surface of high conductive layer in the south Bangong-Nujiang suture is at the depth of about 20 km, which is lower than that in north of Bangong-Nujiang suture. The high conductive layer inside Gandese terrane extends northward and in the southern Qiangtang there exist double high conductive layers. In the upper crust along the profile there are groups of lateral electrical gradient zones or distortion zones of different scale and attitude, indicating the distribution of faults and sutures along the profile. According to the character of electrical structure, the structural characteristic and spatial distribution of Yalung Tsangpo suture, Bangong-Nujiang suture and the major faults of Longmucuo and Ger-Zangbo were inferred.
【Fund】: 国家自然科学基金项目(No4040406);; 北京市重点学科“地球探测与信息技术(XK104910598)”资助
【CateGory Index】: P631.325;P542.5
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