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《QUATERNARY SCIENCES》 1998-03
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GPS SURVEY AND THE RHEOLOGIC STRUCTURES WITH IN THE EASTERN TIBETAN PLATEAU

Chen Zhiliang; Liu Yuping; Zhang Xuanyang; Zhao Jixiang; Tang Wenqing;Deng Changrong; B. C. Burchfiel ;R.W. King ;L. H. Royden( Chengdu Institute of Geology and Mineral Resources , Chengdu 610082; Massachusetts Institute of Technology, Cambridge)  
The crustal inchon of the eastern Tibetan Plateau is the key to understand the collisionand post-collision intracontinental deformation betWeen South China and india, and toresearch the dynamic mechanism and process in Tibetan Plateau.As well-known, the eastern Tibetan Plateau is different from the central TibetMuch of the eastern margin of the Plateau lacks evidence for large-scale young crustalshortening and development of foreland basin, the folds and the thrust faults along theplateau margin are commonly oblique and older than the plateau margin. SinceMiocene,the tectonic frame in the eastern Tibet has been characterized by the wideright-lateral shear zone, which can be subdivided into three units: the weatern beltconsists mainly of a series of NW-trending en echelon right-lateral faults; the centralbelt-a series of NWW-trending en echelon left-latera faults, and the eastern belt-the western margin tectonic belt of the Yangtze block including the Longmenshan faults, the eastern Xianshuihe faults, the Xiaojiang faults, and the Honghe (Red River )faults .Since 1991, a regional GPS netWork has been established along the eastern Tibetan Plateau and its neighbor Sichuan Basin and Yunnan-Guizhou Plateau. The network hasbeen measured at least every two years using multi receivers of dual-frequency instatic relative positioning mode with carrier phase observation . The velocities of thosesites in the Chuan-Dian block and the west of Xianshuihe-Xiaojiang fault aresignificant high,most of them are 5- 10 mm / a relative to Chengdu, in contrast tothe weak movement in the Chuan-Qing and the Yangtze blocks east of the fault.Especially interesting is general clockwise vortex feature of velocity vectors in thesetwo areas. The vortex motion appears to be unrestricted by block boundaries andstrures ; on the contrary, it results in further segmentation within a block and alonga structure . Therefore it is the reflection of rheologic inchon of material in depthrather than those in the upper crust such as a brittle fault slip.Seismic profile research indicates that the thickening of crust in the eastern TibetanPlateau is mainly resulted from the development of lower-velocity layer within themiddle upper crust and the thickening of the lower crust and the contribution of eachof these two processes to the thickening of crust can be as large as 40%. But thedevelOPment of lower-velocity layer is probably an old orogenic process, as indicatedby the fact that most of duchle shear zone in the region is the Miocene or older inage. So, we suggest that the major Process responsible for the young surfacedeformation is a material flow in depth-probably lower crustal flow.The two vortexes structures resulting from the material flow in depth may betentatively named as the Dian -Zang vortex system and the western Sichuan vortexsystem.
【Fund】: 地质矿产部深部地质项目!85-06-214;;美国科学基金!EAR8904096
【CateGory Index】: P548.7
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Chinese Journal Full-text Database 9 Hits
1 An Zhisheng Wang Junda Li Huamei;PALEOMAGNETIC RESEARCH OF THE LOCHUAN LOESS SECTION[J];Geochimica;1977-04
2 Hu HONG-XIANG LU HAN-XING WANG CHUN-YONG HE ZHENG-QIN ZHU LIANG-BAO(Institute of Geophysics, State Seismological Bureau, Beijing) YAN QI-ZHONG FAN YUE-XIN ZHANG GUO-QING DENG YING-E (Seismological Bureau of Yunnan Province, Kunming);EXPLOSION INVESTIGATION OF THE CRUSTAL STRUCTURE IN WESTERN YUNNAN PROVINCE[J];Chinese Journal of Geophysics;1986-02
3 XIONG SIIAO-BAI TENG JI-WBN YIN ZIIOU-XUNLAI MING-HUI HUANG YI-PING (Institute of Geophysics, Academia Sinica);EXPLOSION SEISMOLOGICAL STUDY OF THE STRUCTURE OF THE CRUST AND UPPER MANTLE AT SOUTHERN PART OF THE PANXI TECTONIC BELT[J];Chinese Journal of Geophysics;1986-03
4 Li Jijun Kang Jiancheng (Department of Geography, Lanzhou University);QUATERNARY GLACIATIONS, PHYSIOGRAPHIC STAGES AND LOESS RECORD IN CHINA[J];Quaternary Sciences;1989-03
5 Sun Jie, Xu Chang-fang, Jiang Zhao, Shi Shu-lin, Wang Ji-jun and He Ming(Institute of Geology, State Seismological Bureau);THE ELECTRICAL STRUCTURE OF THE CRUST AND UPPER MANTLE IN THE WEST PART OF YUNNAN PROVINCE AND ITS RELATION TO CRUSTAL TECTONICS[J];Seismology and Geology;1989-01
6 Qiu Zhanxiang(Institute of Vertebrate Paleontology and Paleoanthropology, Academia Sinica) Xie Junyi(The Provincial Museum of Gansu)Yan Defa(Institute of Vertebrate Paleontology and Paleoanthropology, Academia Sinica);DISCOVERY OF SOME EARLY MIOCENE MAMMALIAN FOSSILS FROM DONGXIANG, GANSU[J];Certebrata Palasiatica;1990-01
7 Huang Huafang Peng Zuolin Lu Wei Zheng Jianjing (Lanzhou Institute of Geology , Chinese Academy of Sciences Lanzhou 730000);PALEOMAGNETIC DIVISION AND COMPARISON OF THE TERTIARY SYSTEM IN JIUXI AND JIUDONG BASINS[J];Acta Geologica Gansu;1993-01
8 Qian Fang Xu Shujin (Institute of Geomechanics Chinese Academy of Geology)Chen Fubin Zhao Yongtao (Chengdu Institute of Geography, Academia Sinica);STUDY ON THE PALEOMAGNETISM OF THE XIGEDA FORMATION[J];Journal of Mountain Research;1984-04
9 Kan Rongju(Seismological Bureau of Yunnan Province)Lin Zhongyang(Geophysical Institute, SSB);A PRELIMINARY STUDY ON CRUSTAL AND UPPER MANTLE STRUCTURES IN YUNNAN[J];Earthquake Research In China;1986-04
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