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浅论扬子西南缘卡林型金矿成矿物质来源及有机质在成矿过程中的作用
引用本文:任涛,张兴春,王守旭,冷成彪. 浅论扬子西南缘卡林型金矿成矿物质来源及有机质在成矿过程中的作用[J]. 地质找矿论丛, 2008, 23(4): 287-291,319
作者姓名:任涛  张兴春  王守旭  冷成彪
作者单位:1. 中国科学院地球化学研究所,矿床地球化学国家重点实验室,贵阳,550002;中国科学院,研究生院,北京,100039
2. 中国科学院地球化学研究所,矿床地球化学国家重点实验室,贵阳,550002
摘    要:在前人研究的基础上,对扬子西缘卡林型金矿采用稳定同位素和生物化学试验方法,分析赋金地层中有机质的种类、性质和有机质与金矿的关系,讨论有机质在金元素富集、迁移、成矿过程中的作用.认为赋金地层与后期岩浆热液发生广泛的交换作用,萃取出成矿物质形成成矿流体,这种富含成矿物质的热液流体在一定的条件下富集成矿.

关 键 词:卡林型金矿  有机质  同位素  扬子西南缘
收稿时间:2007-11-13

A TENTATIVE STUDY OF THE MATTER SOURCE AND THE ROLE OF ORGANIC MATTER IN METALLOGENY OF CARLIN-TYPE GOLD DEPOSITS IN SOUTHWESTERN YANGTZE CRATON,SOUTHWESTERN CHINA
REN Tao,ZHANG Xing-chun,WANG Shou-xu and LENG Cheng-biao. A TENTATIVE STUDY OF THE MATTER SOURCE AND THE ROLE OF ORGANIC MATTER IN METALLOGENY OF CARLIN-TYPE GOLD DEPOSITS IN SOUTHWESTERN YANGTZE CRATON,SOUTHWESTERN CHINA[J]. Contributions to Geology and Mineral Resources Research, 2008, 23(4): 287-291,319
Authors:REN Tao  ZHANG Xing-chun  WANG Shou-xu  LENG Cheng-biao
Affiliation:State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, CAS, Guiyang 550002, China;Graduate University of Chinese Academy of Science, Beijing 100039, China;State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, CAS, Guiyang 550002, China;State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, CAS, Guiyang 550002, China;Graduate University of Chinese Academy of Science, Beijing 100039, China;State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, CAS, Guiyang 550002, China;Graduate University of Chinese Academy of Science, Beijing 100039, China
Abstract:Since 1970s,Carlin-type gold deposits have been discovered in the southwestern Yangtze Craton in China.Many predecessors made researches on the ore-forming materials and metallogeny.On basis of the researches this paper applies stable isotope and biochemistry and combines the analysis of the types and nature of organic matter in the ore-bearing strata and studies on the relation between organic matter and gold deposits to discuss the role of organic matter in accumulation and transportation for the gold.A wide-ranging exchange occurred between the ore-bearing strata and the late magmatic hydrothermal fluid with gold-minerals extracted to form Carlin-type gold deposits under certain conditions.
Keywords:Carlin-type gold deposit  organic matter  stable isotope  the southwestern Yangtze Craton
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