RUI Zong-yao1, LU Yan2, LI Guang-ming3, WANG Long-sheng1, WANG Yi-tian1. Looking forward to the prospects of porphyry copper deposits in Tibet[J]. Geology in China, 2003, 30(3): 302-308.
Citation: |
RUI Zong-yao1, LU Yan2, LI Guang-ming3, WANG Long-sheng1, WANG Yi-tian1. Looking forward to the prospects of porphyry copper deposits in Tibet[J]. Geology in China, 2003, 30(3): 302-308.
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Looking forward to the prospects of porphyry copper deposits in Tibet
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1.Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;2. Tibet Bureau of Geology and Mineral Exploration and Development, Lhasa 850000, Tibet, China;3.Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, Sichuan, China
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Abstract
Abstract:Porphyry copper deposits in the world are confined mainly to the Mesozoic-Cenozoic circum-Pacific belt and Paleo-Tethys belt and Paleozoic Central Asia-Mongolian belt, where convergent plates are developed. Tibet is one of the best developed regions of convergent plates in the world, in which the Jinshajiang, Yarlung Zangbo and Nujiang-Bangong Co suture zones lie. These suture zones have a long history of oceanic plate subduction and continent-continent collision with well-developed tectonomagmatic activity marked by widespread plutonic and high-level granite-porphyry, which is favorable to the formation of porphyry copper (-gold) deposits and other related deposits. By referring to the experiences in assessment of porphyry copper deposits at home and abroad in recent years, this paper looks forward to the prospects of porphyry copper deposits in Tibet.
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