青海省某铜矿床地质特征及成因

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英文篇名：Geological characteristics and genesis of a copper deposit in Qinghai 作者：徐龙 ; 张翔 英文作者：XU Long;ZHANG Xiang;Qinghai Geological Survey Bureau; 关键词：乌兰乌珠尔斑岩铜矿 ; 地质特征 ; 矿床 ; 微量元素特征 ; 青海省 英文关键词：Ulam Wu Zhu Er porphyry copper deposit;;geological characteristics;;ore deposit;;trace element characteristics;;Qinghai Province 中文刊名：世界有色金属 英文刊名：World Nonferrous Metals 机构：青海省地质调查局; 出版日期：2019-03-20 13:23 出版单位：世界有色金属 年：2019 期：01 语种：中文; 页：130+132 页数：2 CN：11-2472/TF ISSN：1002-5065 分类号：P618.41

摘要

研究铜矿床地质特征及成因对铜矿床的开发具有重要影响,本文以青海省乌兰乌珠尔斑岩铜矿为例,深入研究了其矿床地质特征和成因,通过研究矿床地质成因发现,青海省乌兰乌珠尔斑岩铜矿的铜矿化主要是由于高温热液蚀变导致的,并且高温热液蚀变越强烈,青海省乌兰乌珠尔斑岩铜矿的铜矿化越好,铜矿化质量越好。
        The study of geological characteristics and genesis of copper deposits has an important influence on the development of copper deposits. Taking Wulan Wuzhur porphyry copper deposit in Qinghai Province as an example, the geological characteristics and genesis of the deposit are studied in depth. It is found that the copper mineralization of Wulan Wuzhur porphyry copper deposit in Qinghai Province is mainly due to high temperature hydrothermal erosion. The stronger the high temperature hydrothermal alteration is, the better the copper mineralization and the better the quality of copper mineralization in Wulan Wuzhur porphyry copper deposit in Qinghai Province.

引文

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    [2]周天健,庞冯秋,汪庆玖,等.铜陵冬瓜山铜矿床60~#线以北深部水文地质特征及防治水措施[J].现代矿业,2018(5):771-772.