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《Acta Geologica Sinica》 2004-04
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Possible Location for Underthrusting Front of the Indus Continent: Constraints from Helium Isotope of the Geothermal Gas in southern Tibet and eastern Tibet

HOU Zengqian, LI Zhenqing Institute of mineral resources, Chinese Academy of Geological sciences, Beijing, 100037  
In order to get deep information on the Tibetan collisional orogen, and to constrain the orogeny processes during Indus—Asian continental collision, the isotopic geochemistry of helium emitted from geothermal springs in the southern Tibetan was systemically studied. Our researches and previously-published data show that the isotope composition of helium have a wide range (R/Ra = 0.017~5.38; R is 3He/4He value of sample, Ra is 3He/4He value of air), which defines two kinds of principal helium variation domains, i.e., mantle helium domain (R/Ra = 0.11~5.38) and crustal helium domain (R/Ra = 0.017~0.072). The former mainly distributes in the Tengchong Rehai geothermal field (R/Ra = 0.40~5.38) near the eastern Himalayan syntax, the Shiquanhe geothermal field (R/Ra = 0.27~0.30) near the western Himalayan syntax, and the Lhasa hydrothermal activity zone (R/Ra = 0.11~0.98) to the east of longitude 89°E. The latter mainly present in the Ngamring hydrothermal activity zone (R/Ra = 0.017~0.072) to the west of 89°E. Near the eastern and western syntaxes, where the hydrothermalism is controlled by large-scale strike-slip faults, there are 50% mantle-derive helium's contribution in geothermal helium. While in the hinterland of the plateau, where NS-trending rift control the development of hydrothermal zone, the value of R/Ra has obvious variation in east—west direction rather than in south—north direction. Both two helium domains are bounded by longitude 89°E in EW-direction, but all bestride the Yarlung Zangbu suture in SN-direction. Synthetic analysis on the helium isotopic data and available geophysical data shows that modern hydrothermal activity was mainly driven by magmatic chambers or partially molten layers occurring as patches in the upper crust, but the contribution of mantle heat and mass (helium) to spring gases has been recognized to the east of 89°E. As a consequence, we proposed that the Indus continent is underthresting obliquely northwards as a whole with an inconsistent underthrusting front, which shows different slab styles in two sides of 89°E. To the west of 89°E, the continental slab downgoing towards NNE in a gentle slope has probably passed the Yarlung Zangbu suture and reached to the Bangong—Nujing suture; while to the east of 89°E, underthrusting slab front, likely to tear down along the Yadong—Gulou rift valley, is downgoing in a steep slope, thus has not spanned the Yarlung Zangbu suture.
【Fund】: 国家重点基础研究规划 973项目“印度 -亚洲大陆主碰撞带成矿作用”(编号 2 0 0 2 CB412 610 )的成果
【CateGory Index】: P542
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9 CHEN Chao1,NIU Shu-yin1,WANG Bao-de1,SUN Ai-qun1,MA Bao-jun1,WANG Wen-xue2,GAO Yin-cang2(1.Shijiazhuang University of Economics,Shijiazhuang 050031,Hebei,China;2.Geological Research Party of Shijiazhuang,Shijiazhuang 050081,Hebei,China);A tentative discussion on ore-forming material sources and mineralization of the Shihu gold deposit in western Hebei Province[J];Geology in China;2009-06
10 CHEN You-shun1,FANG Hou-guo2,LIU Ping-hui3,LI Shan-ping4,LI Zhi-min1(1.Qinghai Seismological Bureau,Xining 810001;2.Yellow River Conservancy Committee,Zhengzhou 450003;3.North China Institute of Water Conservancy and Hydroelectric Power,Zhengzhou 450011;4.Salt Lake Institute,Chinese Academy of Sciences,Xining 810008,China);Distribution,Formation and Exploitation of Mineral Resources in Qinghai-Tibet Plateau[J];Geography and Geo-Information Science;2009-06
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1 XIAO Wen-jiao~1,SHU Liang-shu~2,GAO Jun~1,XIONG Xiao-lin~3,WANG Jing-bin~4, GUO Zhao-jie~5,LI Jin-yi~6,SUN Min~7 (1.State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences, Beijing 100029,China;2.Department of Earth Sciences,Nanjing University,Nanjing,Jiangsu,210093,China;3.Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou,Guangdong,510640,China;4.Institute of Geology and Mineral Resources,Beijing 100012,China;5.Department of Earth and Space Sciences,Nanjing University, Nanjing,Jiangsu,210093,China;6.Institute of Geology,Chinese Academy of Geological Sciences,Beijing,100037,China; 7.Department of Earth Sciences,The University of Hong Kong,Pokfulam Road,Hong Kong,China);CONTINENTAL DYNAMICS OF THE CENTRAL ASIAN OROGENIC BELT AND ITS METALLOGENY[A];[C];2009
2 XIAO Bo~(1,2,3),LI GuangMing~(1,2),QIN KeZhang~(1,2),LI JinXiang~(1,2),ZHAO JunXing~(1,2,3),LIU XiaoBing~(3,4), XIA DaiXiang~5,WU XingBing~5 and PENG ZhenWei~6 (1 Institute of Geology and Geophysics,CAS,Beijing 100029,China;2 Key Lab of Mineral Resources,Institute of Geology and Geophysics,CAS,Beijing 100029,China;3 Graduate University of Chinese Academy of Sciences,Beijing 100049,China; 4 Institute of Tibetan Plateau Research,CAS,Beijing 100085,China;5 Tibet Ju Long Copper Ltd.,Lhasa 850030,Tibet, China;6 Department of Geology,Moscow State University,Moscow 11923,Russia);Magmatic intrusion center and mineralization center of Qulong porphyry Cu-Mo deposit in Tibet:Evidence from fissure-veinlets and mineralization intensity[A];[C];2009
3 WU Huaying,ZHANG Lianchang,CHEN Zhiguang and WAN Bo 1.Key laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Graduate School of Chinese Academy of Sciences,Beijing 100049,China;Geochemistries,tectonic setting and mineralization potentiality of the ore-bearing monzogranite in the Kulitu molybdenum(copper) deposit of Xar moron metallogetic belt,Inner Mongolia.[A];[C];2009
4 ZHANG Qi,WANG Yuan-long,JIN Wei-jun,JIA Xiu-qin,LI Cheng-dong 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China; 2.Institute of High Energy Physics,Chinese Academy of Sciences,Beijing 100039,China; 3.Tianjin Institute of Geology and Mineral Resources,Tianjin 300170,China;Criteria for the recognition of pre-,syn-and post-orogenic granitic rocks.[A];[C];2009
5 ZHANG Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing,100029,China);Adakite research:retrospect and prospect[A];[C];2009
6 ZHAO Wen-jin(Chinese Academy of Geological Sciences, Beijing 100037,China);Advances in continental dynamics research in China:Commemorating the 60th anniversary of the founding of the Chinese geophysical society[A];[C];2007
7 L(u|¨)Yan~(1,3*) Ni Sidao~(2,1) Liu Bin~1 Sun Youshun~3 1.School of Earth and Space Sciences,University of Science and Technology of China,Hefei,230026,China 2.Key Laboratory of Dynamical Geodesy,Institute of Geodesy and Geophysics,Wuhan,430077,China 3.Department of Earth,Atmospheric and Planetary Sciences,Massachusetts Institute of Technology, Cambridge,Massachusetts 02139,USA;Pn Tomographic Velocity and Anisotropy beneath Western China and the Surrounding Region[A];[C];2011
8 He Rizheng Gao Rui Zheng Hongwei;The research of E-W trend tectonics in Tibetan Plateau[A];[C];2011
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8 LIU BAO-CHENG TONG WEI ZHANG BAO-SHAN(Departments of Geophysics and Geology, Peking University, Beijing)ZHANG LI-MIN(Institute of Geophysics, Academia Sinica, Beijing)ZHANG ZHAO-XING (Seismological Office, Tengchong County, Yunnan Province);MICROSEISMIC OBSERVATION IN TENGCHONG VOLCANO-GEOTHERMAL REGION[J];Chinese Journal of Geophysics;1986-06
9 MU ZHI-GUO TONG WEI(Department of Geology, Peking University, Beijing, China)GARNISS H. CURTIS(Department of Geology & Geophysics, University of California, Berkeley, CA 94720, U. 5. A.);TIMES OF VOLCANIC ACTIVITY AND ORIGIN OF MAGMA IN TENGCHONG GEOTHERMAL AREA,WEST YUNNAN PROVINCE[J];Chinese Journal of Geophysics;1987-03
10 WANG CHUN-YONG; ZHANG XIAN-KANG; DING ZHI-FENG; RUAN HONG; DENG HONG-ZHAO (Institute of Geophysics, State Seismological Bureau, Beijing 100081, China)(Geophysical Prospecting Center, State Ceismological Bureau,Zhengzhou 450003, China);FINITE-DIFFERENCE TOMOGRAPHY OF UPPER CRUSTAL STRUCTURE IN DABIESHAN OROGENIC BELT[J];Chinese Journal of Geophysics;1997-04
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