引用本文:李定谋, 李保华.云南哀牢山金矿床的成矿条件[J].沉积与特提斯地质,2000,(1):60-77.[点击复制]
[点击复制]
【打印本页】 【在线阅读全文】【下载PDF全文】 查看/发表评论下载PDF阅读器关闭

←前一篇|后一篇→

过刊浏览    高级检索

本文已被:浏览 400次   下载 210 本文二维码信息
码上扫一扫!
云南哀牢山金矿床的成矿条件
李定谋,李保华
0
(1. 成都地质矿产研究所, 四川 成都 610082;
2. 成都理工学院, 四川 成都 610059)
摘要:
成矿作用包括成矿物质的来源、搬运及沉淀的全过程,其中最活跃的因素为成矿流体。可以说,没有流体就不会形成矿床,但也不是所有流体都成矿。笔者通过哀牢山蛇绿混杂岩带典型金矿床的物质组成、成矿规律、蚀变及控矿作用的研究,对哀牢山金矿带的成矿流体来源,成矿流体动力学、地球化学及物理化学性质进行了详细地讨论;对金矿的成矿物质来源,金在成矿流体中的存在形式,迁移过程中平衡、失稳-沉淀等进行了详细地分析和探讨。
关键词:  成矿流体  水动力分析  地球化学系统  金矿  哀牢山
DOI:
附件
投稿时间:1999-03-08
基金项目:
The mineralization of the gold deposits in the Ailao Mountains, Yunnan
LI Ding-mou, LI Bao-hua
(1. Chengdu I nstitute of Geology and Mineral Resources, Chengdu 610082, China;
2. Chengdu University of Technology, Chengdu 610059, China)
Abstract:
The Mineralization is referred to as all the processes of the origin, transport and precipitation of ore-forming matter. The ore-forming fluids are apparently very significant in the formation of ore deposits although not all of them can lead to the formation of ore deposits. The present paper deals in detail with the origin, dynamics, geochemistry and physicochemistry of the ore-forming fluids, in combination with the origin of ore-forming matter, gold behaviour in the ore-forming fluids, equilibrium and unstability-precipitation in the course of migration on the basis of mineral composition and mineralization, alteration and ore-controlling factors of the representative gold deposits hosted in the Ailao Mountains ophiolitic melange belt, Yunnan.
Key words:  ore-forming fluid  hydrody namics  geochemical system  gold deposit  Ailao Mountains

用微信扫一扫

用微信扫一扫