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《Chinese Journal of Geophysics》 1991-05
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INTEGRATED INVESTIGATIONS OF THE QINGHAI-TIBET PLATEAU ALONG THE YADONG-GOLMUD GEOSCIENCE TRANSECT

Wu GONG-JIAN GAO Rui Yu QIN-FAN CHENG QING-YON MENG LING-SHUN DONG XuE-BIN CHUI ZUO-ZHOU YIN ZHOU-XUN SHEN XIAN-JIEZHOU YAO-XIU et al. Lithospheric Research Centre, CAGS, Beijing 100037,China University of Geosciences, Beijing 100083,Changchun College of Geoloy, Changchun, 130026,562 Comprehensive Research Brigade, CAGS,Institute of Geophysics, Academia Sinica, Beijing 100101,Institute of Geology, Academia Sinica, Beijing 100029,Aeromagnetic Survey, Ministry of Geol. & Min. Res. Beijing 100083.  
In addition to the previous work, we have done the following geophysical measurements: paleomagnetic measurement on 2000 samples, gravity profiling from Lhasa to Golmud, magnetic profiling from Yadong to Golmud, MT measurement (period: 0.01-10000s) and heat flow survey (12 values obtained). Image processing has been carried out with respect to the regional gravity and magnetic anomalies. Seis-81 are used to reinterpret the available seismic data. An interactive system incorperating seismic, gravity, magnetic and MT data is developed to set up a geophysical model for the Qinghai-Tibet Plateau.based on the preliminary results, we obtained the following conclusions: 1. Qinghai-Ti-bet Plateau consists of six terranes which seperated from Gonwana during Paleozoic and Me-sozoic successively, and latter accreted and united to the margih of the Eurasian continent at different erogenic times; 2. The tectonics of the southern and northern parts of the Plateau are different if the Ando-Dengqen fault is taken as a boundary. In the south, the lithosphere is more active, the crust is thick and the upper mantle making up the lithosphere is thin, and there exist two layers of high conductivity and low velocity. The crust is hot, and the collision time is later than that of the northern part of the Plateau. The lithosphere of the northern part, on contrast, is relatively stable, both the crust and the upper mantle are thick. The layer of low velocity and high conductivity is located at a shallow depth. The crust here is relatively cool, and the collision of the blocks took place earlier; 3. The slant of earhquake focus plane shows that the Plateau is mainly suffering the compression of the Idian plate and the resistance of the Eurasian plate, or the stress from the north. This results in the thicken-ing and shortening, and consequently the uplifting of the Qinghai-Tibet Plateau; 4. In comparison with the Andes orogenic belt(subduction) and the Alps orogenic belt (obduction and overlaping), the Qinghai-Tibet Plateau is a new type of orogenic belt characterized by obduction and overlaping, as well as subduction.
【Fund】: 国家自然科学基金;; 地质矿产部共同资助的课题
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6 TENG Ji-wen 1.College of GeoExploration Science and Technology,Jilin University,Changchun 130026,China 2.Institute of Geology and Geophysics, Chinese Academy of Science, Beijing 100029,China;Research on Layer-Bundle Fine Structures and Physical Attributes of Crust-Mantle Boundary in Deep Earth[J];Journal of Jilin University(Earth Science Edition);2006-01
7 TENG Ji-wen~ 1,2 1. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029,China 2. College of GeoExploration Science and Technology, Jilin University, Changchun 130026,China$$$$;The Developmental Trends of the Contemporary Geophysics and the Tasks in Research Process of Systemic Geosciences in China[J];Journal of Jilin University(Earth Science Edition);2006-05
8 TENG Ji-wen1,2,LIU Jian-ming2,LIU Cai1,YAO Jing-jin3,HAN Li-guo1,ZHANG Yong-qian21.College of GeoExploration Science and Technology,Jilin University,Changchun 130026,China2.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China3.Chinese Academy of Geological Sciences,Langfang,Hebei 102849,China;Prospecting for Metal Ore Deposits in Second Deep Space of Crustal Interior,the Building of Strategy Reserve Base of Northeast China[J];Journal of Jilin University(Earth Science Edition);2007-04
9 TENG Ji-wen1,2,LIU Cai2,HAN Li-guo2,RUAN Xiao-min1,YAN Ya-fen1,ZHANG Yong-qian11.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China2.College of GeoExploration Science and Technology,Jilin University,Changchun 130026,China;The Dynamical Mechanism for Medium Rapture and Motion of Deep Matler on Wenchuan-Yingxiu M_S8.0 Earthquarce,2008[J];Journal of Jilin University(Earth Science Edition);2009-04
10 LIAN Yong-lao1,2,CAO Xin-zhi1,YAN Chang-hai3,DU Xin31.Faculty of Resources,China University of Geosciences,Wuhan 430074,China2.No.1 Gold Geological Party of CAPF,Mudanjiang,Heilongjiang 157021,China3.Henan Institute of Geological Survey,Zhengzhou 450007,China;Exhalative Sedimentary Genesis of Lawu Copper-Lead-Zinc Deposit in Dangxiong County of Tibet[J];Journal of Jilin University(Earth Science Edition);2010-05
China Proceedings of conference Full-text Database 10 Hits
1 WANG Hai-Long~(1,2),HUANG Bao-Chun~(1*),QIAO Qing-Qmg~1,CHEN Jun-Shan~1 1 State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences, Beijing 100029,China 2 Research Institute of Petroleum Exploration and Development-Northwest,PetroChina,Lanzhou 730020,China;Paleomagnetic study on Cretaceous and Paleogene rocks from eastern Heilongjiang,NE China and its tectonic implications[A];[C];2012
2 TENG Ji-Wen~(1,2),ZHANG Hong-Shuang~1,SUN Ruo-Mei~1,YAN Ya-Fen~1,ZHANG Xue-Mei~1, YANG Hui~1,TIAN You~1,ZHANG Yong-Qian~1,RUAN Xiao-Min~1 1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2 Jilin University,Changchun 130026,China;Geophysical field characteristics and dynamic response of segmentations in East-west direction and their boundary zone in central Tibetan plateau[A];[C];2012
3 ZHANG Yong-Qian~1,TENG Ji-Wen~1,WANG Fu-Yun~2,ZHAO Wen-Zhi~3, LI Ming~3,WANG Qian-Shen~1 1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2 Geophysical Exploration Center,China Earthquake Administration,Zhengzhou 450002,China 3 SINOPEC Research Institute of Petroleum Exploration and Development,Beijing 100083,China;Structure of the seismic wave property and lithology deduction of the upper crust beneath the Yinshan orogenic belt and the northern Ordos block[A];[C];2012
4 Zhongjie Zhang~(a,*),Yangfan Deng~(b,c),Jiwen Teng~a,Chunyong Wang~d,Rui Gao~e,Yun Chen~a,Weiming Fan~b a State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China b Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China c Graduate University of Chinese Academy of Sciences,Beijing 100049,China d Institute of Geophysics,China Earthquake Administration,Beijing 100081,China e Institute of Geology,Chinese Academy of Geological Sciences,Ministry of Land and Resources,Beijing 100037,China;An overview of the crustal structure of the Tibetan plateau after 35 years of deep seismic soundings[A];[C];2012
5 Ma Gengjie,Liu Guofan,Liu Qin'an,Zhou Wenbo,Liu Weijie (No.1 Geology Engineering Instiute,Henan Provincial Bureau of Geo-exploration and Mineral Development,Zhumadian 463000,Henan,China);Geological Characteristics and Ore Prospects of Gold Deposit in Xixia Gaozhuang Henan[A];[C];2010
6 Liu Guofan,Ma Gengjie,Liu Qin'an,Zhou Wenbo,Zhang Fengrui,Liu Weijie (No.1 Geology Engineering Instiute,Henan Provincial Bureau of Geo-exploration and Mineral Development,Zhumadian 463000,Henan,China);Geoloical Characteristics and Prospecting Prospectc of the Tiaoshan Iron Deposit in Biyang,Henan[A];[C];2010
7 TENG Ji-wen (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100101,China);GREAT ACHIEVEMENTS IN GEOPHYSICS IN THE 20TH CENTURY AND DEVELOPING FRONTIERS FOR THE 21ST CENTURY[A];[C];2003
8 YE Zheng-Ren WANG Jian Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;DYNAMICS OF PRESENT-DAY CRUSTAL MOVEMENT IN THE CHINA MAINLAND[A];[C];2004
9 YAN Yong-Li~1,MA Xiao-Bing~1,YUAN Guo-Ping~2,LI Yuan-Hou~3,KONG Xiang-Ru~1 1 Institute of Geology and Geophysics,Chinese Academy of Science,Beijing 100029,China 2 Geological Institute of Oilfield Company of Zhejiang,Hangzhou 310013,China 3 Institute of Geophysical and Geochemical Exploration,Langfang 065000,China;Application of magnetotelluric method in groundwater pollution detection on Asuwei refuse sanitary landfill[A];[C];2008
10 ZHANG XueMei~(1+),SUN RuoMei~1 &TENG JiWen~(1,2) 1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China; 2 College of Geo-exploration Science and Technology,Jilin University,Changchun 130026,China;Study on crustal,lithospheric and asthenospheric thickness beneath the Qinghai-Tibet Plateau and its adjacent areas[A];[C];2008
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 Wang Hongzhen;ON THE GEOTEC TONIC UNITS OF XIZANG (TIBET) REGION[J];;1983-01
2 TENG CHI-WEN AND OTHERS (Institute of Geophysics, Academia Sinica);DEEP REFLECTED WAVES AND THE STRUCTURE OF THE EARTH CRUST OF THE EASTERN PART OF CHAIDAM BASIN (柴达木东盆地)[J];Chinese Journal of Sinica;1974-02
3 CHEN YUN-TAI;LIN BANG-HUI;LI XING-CAI;WANG MIAO-YUEInstitute of Geophysics, Academia SinicaXIA DA-DE;WANG XING-HUIThe Seismological Brigade of Chengdu, National Seismological BureauLIU WAN-QIN;LI ZHI-YONGInstitute of Geophysics, Academia Sinica;THE DETERMINATION OF SOURCE PARAMETERS FOR SMALL EARTHQUAKES IN QIAOJIA (巧家) AND SHIMIAN (石棉) AND THE ESTIMATION OF POTENTIAL EARTHQUAKE DANGER[J];Chinese Journal of Sinica;1976-03
4 CHANG LI-MIN YAO ZHEN-XING(Institute of Geophysics, Academia Sinica);THE Q-VALUE OF THE MEDIUM OF THE TIBETAN PLATEAU AROUND LASA REGION[J];Chinese Journal of Sinica;1979-03
5 Teng Ji-wen Wang Shao-zhou Yao Zhen-xingXú Zhen-wǔ Zhu Zhi-wen Yang Bing-ping Zhou Wen-hu (Institute of Geophysics, A oademia Sinica);CHARACTERISTICS OF THE GEOPHYSICAL FIELDS AND PLATE TECTONICS OF THE QINGHAI-XIZANG PLATEAU AND ITS NEIGHBOURING REGIONS[J];Chinese Journal of Geophysics;1980-03
6 Huan Wen-lin Wang Su-yun Shi Zhen-liang Yan Jia-quan(Institute of Geophysics, State Seismological Bureau);THE DISTRIBUTION OF EARTHQUAKES FOCI AND PLATE MOTION IN THE QINGHAI-XIZANG PLATEAU[J];Chinese Journal of Geophysics;1980-03
7 Zhang Li-min Shu Pei-yi Yang Bing-ping Zhang Zhi-he(Institute of Geophysics, Academia Sinica);THE AVERAGE STRESS FIELDS OF ZHAMO AND DAMXUNG REGIONS IN THE XIZANG PLATEAU[J];Chinese Journal of Geophysics;1980-03
8 Feng Rui He Zheng-qin (Institute of Geophysics, State Seismological Bureau);Q-VALUE FOR SURFACE WAVES IN THE EASTERN REGION OF XIZANG PLATEAU[J];Chinese Journal of Geophysics;1980-03
9 ZHU ZHI-WEN ZHU XIANG-YUAN ZHANG YI-MING (Institute of Geophysics, Academia Sinica);PALAEOMAGNETIC OBSERVATION IN XIZANG AND CONTINENTAL DRIFT[J];Chinese Journal of Geophysics;1981-01
10 YANG BING-PING SHU PAI-YI ZHANG ZHI-HE (Institute of Geophysics, Academia Sinica);SOME CHARACTERISTICS OF SMALL EARTHQUAKES IN THE ZHAMO AND DAMXUNG DISTRICTS OF THE XIZANG PLATEAU[J];Chinese Journal of Geophysics;1981-01
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