新疆查汗沙拉锑矿床地质特征及成因分析

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英文篇名：Geological characteristics and genetic analysis of chahan shashi antimony deposit in xinjiang 作者：罗耀鸿 英文作者：LUO Yao-hong;First Regional Geological Survey Brigade of Xinjiang Geological and Mineral Bureau; 关键词：锑矿床 ; 地质特征 ; 矿带 英文关键词：antimony deposit;;Geological features;;Ore belt 中文刊名：COLO 英文刊名：World Nonferrous Metals 机构：新疆地矿局第一区域地质调查大队; 出版日期：2019-05-24 11:38 出版单位：世界有色金属 年：2019 期：No.521 语种：中文; 页：COLO201905128 页数：2 CN：05 ISSN：11-2472/TF 分类号：222-223

摘要

新疆查汗沙拉锑矿床位于西南天山中部的萨阿尔明晚古生代沟弧带的西段,它与萨瓦亚尔顿金锑银矿、卡拉脚古牙锑金矿、古勒克达坂卡堤锑金矿构成查汗沙拉锑金矿带。矿区总体受控于一大型逆冲推覆构造带,处于查汗沙拉锑异常区浓集中心域内,矿体产于阿尔腾克斯组含炭碎屑岩中,显示多元素多期次的成矿特征.成矿物质来自于赋矿地层,成矿热液则是由岩浆水和天水组成的混合水,属沉积改造型锑银多金属矿床.
        The chahan shala antimony deposit is located in the western part of the late Paleozoic gully arc belt in the middle of tianshan mountain in southwest China. Overall mining area is controlled by a large thrust nappe tectonic belt, check in sweat salad sb abnormal area thick concentrated heart domain, orebody in al teng, groups of clastic rock containing carbon shows that metallogenic characteristics of many elements much issue. Ore-forming material comes from the ore formation,ore-forming hydrothermal is the mixed water composed of magma water and tianshui, sedimentary transformation type of antimony silver polymetallic deposit.

引文

[1]付王伟,于明杰,毛启贵,etal.新疆小石头泉地区黄草沟银多金属矿地质特征及矿床成因[J].矿产勘查,2018,9(2):273-278.