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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2011-01
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Composition of single melt inclusion in quartz phenocryst in the Jiama Cu-polymetallic Deposit,Tibet

ZHOU Yun1,WANG Xiong-wu1,TANG Ju-xing2,QIN Zhi-peng2,PENG Hui-juan2,LI Ai-guo3,YANG Ke3,WANG Hua3,LI Jiong3,ZHANG Ji-chao3 1.This Pape Studies College of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China;2.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China;3.Shanghai Institute of Applied Physics,Chinese Academy of Sciences,Shanghai 201204,China  
the relation of magmatic crystallization,evolution and hydrothermal transition to mineralization.Linkman TS1500 heating stage is used to characterize the melt inclusions in the quartz phenocryst of the ore-bearing porphyry in the Jiama Cu-polymetallic deposit and to measure their homogenization temperatures,while EMPA and SRXRF micro-probe are used to measure the major and trace elements of the melt inclusions.The formation temperature of the ore-bearing porphyry is 630~880℃.Na and Ca tend to be rich in magmatic volatile,and the volatile develops into hyperthermal and hypersaline fluids as it becomes saturated and exsolutioned.The metallogenic elements selectively force into the gas-phase of volatile from the earliest crystallization stage,and the metallogenic elements are preliminarily enriched in the exsolutioned volatile.A conclusion is arrived that the genesis of the deposit is closely related to magmatic hydrothermal mineralization in the porphyry-skarn system.
【Fund】: 科技部行业专项协作项目(200911007-12);; 地保工程项目(1212010012005);; 青藏专项项目(1212010818089);; 西藏华泰龙矿业开发有限公司勘探项目、技术开发项目(E0804);; 教育部岩石学矿床学国家重点(培育)学科建设基金资助项目(SZD0407)
【CateGory Index】: P618.41
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