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矿床及其组合是地壳演化的标志物──右江幔隆的发生、发展与滇黔桂卡林型金矿关系探讨
引用本文:范军,肖荣阁.矿床及其组合是地壳演化的标志物──右江幔隆的发生、发展与滇黔桂卡林型金矿关系探讨[J].矿物学报,1997(4).
作者姓名:范军  肖荣阁
作者单位:中国建筑材料工业地质勘查中心贵州总队!贵阳,550008,中国地质大学!北京,100083
基金项目:中国科学院矿床地球化学开放研究实验室资助
摘    要:现代金成矿地球动力学的研究,揭示了矿床及其组合与构造变动、岩浆活动一样,是地壳变革的一个事件,因此从成矿环境地质方面可反演矿床及其组合的形成史,正确划分出与区域地壳演化阶段相适应的矿化类型;滇黔桂卡林型金矿的形成与右江幔隆的发生、发展息息相关,本文借用金成矿地球动力学的一些思想,用地幔隆起的观点分析了本区卡林型金矿的形成。

关 键 词:金成矿地球动力学  右江幔隆  卡林型金矿  滇黔桂地区

ORE DEPOSITS AND THEIR ASSEMBLAGES ARE THE MARKERS OF EARTH'S EVOLUTION
Fan Jun ,Xiao Rongge..ORE DEPOSITS AND THEIR ASSEMBLAGES ARE THE MARKERS OF EARTH'S EVOLUTION[J].Acta Mineralogica Sinica,1997(4).
Authors:Fan Jun  Xiao Rongge
Institution:Fan Jun ,Xiao Rongge1.
Abstract:Modern geodynamic studies of gold metallogenesis has revealed that the ore deposits and their assemblages, like tectonic changes and magmatic activities, are a kind of geological events during the evolution of the Earth. Therefore,the geological environment of metallogenesis can reflect the history of formation of ore deposits and their assemblages. On this basis, the mineralization types corresponding to the evolution stages of a regional crust can be correctly distinguished.The Carlin-type gold deposits in the Yunnan-Guizhou-Guangxi area are closely genetically connected with the generation and development of the Youjiang mantle uplift. This paper analyses the mechanism of formation of the Carlin-type gold deposits in this area in terms of the modern geodynamic data on gold metallogenesis and from the view of point of mantle uplift.
Keywords:geodynamics of gold metallogenesis  Youjiang mantle uplift  Carlin-type gold deposits  Yunnan-Guizhou-Guangxi area
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