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《Earth Science Frontiers》 2003-03
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SUBDUCTION OF INDIA BENEATH TIBET:MAGMATISM EVIDENCE

ZHAO Zhi-dan~(1,2),MO Xuan-xue~(1,2),LUO Zhao-hua~(1,2),ZHOU Su~3,DONG Guo-chen~1,WANG Liang-liang~1,ZHANG Feng-qin~1(1.School of Earth Science and Mineral Resources, China University of Geosciences,Beijing 100083, China; 2.China University of Geosciences Key Laboratory of Lithospheric,Deep-level process and Exploration, Ministry of Education, Beijing 100083, China;3.The Geological Lab Center, China University of Geosciences, Beijing 100083, China)  
The northward subduction of India plate beneath Tibet followed the onset of India collided with Asia is one of the most fundamental questions to the evolution of Tibetan plateau. But it is still in debate. Recently, increasing geophysical studies favor the model that India has subducted beneath Asia to the depth of 200 km beneath the plateau to the Banggong-Nujiang suture. Age, petrology and geochemistry of the wide-spreading postcollisional magmatism in Tibetan plateau allow us to reveal the composition and processes of the plateau's lithosphere after India collided with Asia around 55 Ma ago. Our results suggest that the Gangdese belt is geochemically a part of the north Tibet (Qiangtang, Kunlun, Hoh Kil). North Tibet has an undisturbed, ancient enriched upper mantle source region. Isotopic geochemistry evidence show that India has subducted beneath Gangdese to the north of Yarlung Zangpo suture 13~25 Ma ago. Taking the northward ongoing motion of India into account, we conclude that India plate should have subducted beneath Tibet to Bangong-Nujiang suture at present-day. This model agree very well with the results of helium geochemistry of spring water from southern Tibet and some geophysical survey got recently.
【Fund】: 国家自然科学基金资助项目 (4 0 10 3 0 0 3 ) ;; 国家重点基础发展规划项目 (G19980 40 80 0 2 0 0 2CB412 60 0 ) ;; 国土资源部青藏专项计划 (2 0 0 10 10 2 0 40 1);; 重点基础资助项目 (95 0 110 1 3 )
【CateGory Index】: P542
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4 Huang Baochun~1,Zhou Yaoxiu~2,Zhu Rixiang~1 1.State Key Laboratory of Lithosphere Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029, China 2.Aeromagnetic and Remote Sensing Center,Ministry of Land and Resources,Beijing 100083,China;Discussions on Phanerozoic evolution and formation of continental China,based on paleomagnetic studies[A];[C];2009
5 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
6 CHEN ZhiGuang,ZHANG LianChang,WAN Bo,ZHANG YuTao and WU HuaYing 1.Key laboratory of Mineral Resources,Institute of Geology and Geophysics,CAS,Beijing 100029,China 2.State key laboratory of lithospheric evolution,Institute of Geology and Geophysics,CAS,Beijing 100029,China 3.Graduate School of Chinese Academy of Sciences,Beijing 100039,China;Geochemistry and geological significances of ore-forming porphyry with low Sr and Yb value in Wunugetushan copper-molybdenum deposit,Inner Mongolia.[A];[C];2009
7 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
8 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
9 ZHANG Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing,100029,China);Adakite research:retrospect and prospect[A];[C];2009
10 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
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