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湘黔地区内生金矿分布规律的探讨
引用本文:叶大元,张瑞蓉.湘黔地区内生金矿分布规律的探讨[J].贵州工业大学学报(自然科学版),1991(3).
作者姓名:叶大元  张瑞蓉
作者单位:贵州工学院地质系,贵州工学院地质系
基金项目:国家自然科学基金项目:《湘黔地区内生金矿控矿条件及远景预测》的部分成果
摘    要:湘黔地区内生金矿的形成和时空分布,受中晚元古代以来发育于川中古陆东南活动边缘古板块俯冲带制约。这种制约表现为俯冲、碰撞,并多次向洋迁移和与之伴随的构造—岩浆活动。从而在容矿地层层位、成矿时间跨度、矿床类型、矿物组合、元素组合、金的赋存形式、金的成色以及与岩浆岩的关系等方面,从西北向东南呈现规律性变化。

关 键 词:金矿  分布规律  湘黔地区

A Study on The Distribution Law of Gold Deposit In Hunan And Guizhou
Ye Dayuan Zhang Ruirong.A Study on The Distribution Law of Gold Deposit In Hunan And Guizhou[J].Journal of Guizhou University of Technology(Natural Science Edition),1991(3).
Authors:Ye Dayuan Zhang Ruirong
Institution:Department of Geology
Abstract:The formation and distribution of gold mineral deposits in Hunan and Guizhou are restrained by the old plate subduction zone developing on the active continental margin in the middle of Sichuan Oldland of mid-lat Proterozoic. The Restraint is embodied in plate subdtction, collision and the repeated movements towards the ocean and the accompanied structural-magmatic activities. The ore-bearing layey location, metallogenetic time-span, gold deposit type, mineral combination, element combination, existing form, relative purity of gold and the relationship between gold deposit and magmatic rock all change regularily from northwest to suntheast.
Keywords:gold deposit  distribution law  distribution of mineral deposit  magma  
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