浅析红石铜矿地质特征及矿床成因

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英文篇名：Brief Analysis of Geological Characteristics and Genesis of Hongshi Copper Deposit 作者：李新川 英文作者：LI Xin-chuan;Xinjiang Baodi Mining Co., Ltd.; 关键词：红石铜矿床 ; 地质特征 ; 矿床成因 英文关键词：rutile copper deposit;;geological characteristics;;genesis of the deposit 中文刊名：世界有色金属 英文刊名：World Nonferrous Metals 机构：新疆宝地矿业股份有限公司; 出版日期：2019-05-24 11:38 出版单位：世界有色金属 年：2019 期：05 语种：中文; 页：146+148 页数：2 CN：11-2472/TF ISSN：1002-5065 分类号：P618.41

摘要

红石铜矿地处东天山大南湖-头苏泉岛弧带北段的卡拉塔格地区。矿体产于奥陶系大柳沟组火山岩中,呈脉状产出,区内构造对矿体起着明显的控制作用。该区褶皱与断裂构造比较突出,侵入岩较发育,具有非常优越的成矿地质条件,找矿潜力巨大,因此成为研究的热点。该矿矿床成因为中低温火山热液型铜矿床。下文结合实践对该矿地质特征进行分析的基础上探讨其矿床成因,以供参考。
        The Hongshi copper deposit is located in the Karatag area of the northern part of the Dananhu-Tousuquan Island arc belt in the eastern Tianshan Mountains. The ore bodies occur in the volcanic rocks of the Ordovician Daliugou Formation and are vein-like. The structure in the area plays an obvious role in controlling the ore bodies. The folds and faults in this area are prominent, the intrusive rocks are well developed, and they have excellent metallogenic geological conditions.They have great potential for prospecting. Therefore, they have become a research hotspot. The genesis of the deposit is a medium-low temperature volcanic hydrothermal copper deposit. Based on the analysis of the geological characteristics of the deposit, the genesis of the deposit is discussed for reference.

引文

[1]姬金生,陶洪祥,曾章仁,等.东天山康古尔成矿带地质分析[J].北京:地质出版社,2016,(12).
    [2]宋会侠,刘玉琳,屈文俊,宋彪,张锐,成勇.新疆红石铜矿矿床地质特征[J].岩石学报,2017,(03).