新疆阿克陶县得克铅锌矿地球化学成矿特征及成因浅析

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英文篇名：Geochemical mineralization characteristics and genesis of deke lead-zincl deposit in Aktao county, XinJiang 作者：唐龙元 ; 王学杰 ; 杨秉飞 英文作者：TANG Long-yuan;WANG Xue-jie;YANG Bing-fei;Xinjiang Geological Exploration Institute, General Administration of Metallurgical Geology of China; 关键词：得克铅锌矿 ; 地质特征 ; 地球化学特征 ; 成因 英文关键词：Deke lead-zinc deposit;;geological characteristics;;geochemical characteristics;;genesis 中文刊名：COLO 英文刊名：World Nonferrous Metals 机构：中国冶金地质总局新疆地质勘查院; 出版日期：2019-07-09 16:40 出版单位：世界有色金属 年：2019 期：No.525 语种：中文; 页：COLO201909085 页数：2 CN：09 ISSN：11-2472/TF 分类号：151+153

摘要

得克铅锌矿是新疆地区发现的一重要的铅锌矿床,分布新疆阿克陶县境内,矿化以铅锌矿为主,矿床赋存于中上古生代坳陷沉积的一套浅变质的海相或海陆交互相的碳酸岩-碎屑岩建造地层中,矿石结构简单,主要为他形不规则粒状及片状,矿石构造为浸染状和脉状。文章对该矿地球化学特征进行分析,探讨其矿床成因,认为该矿成因类型属于层控热液改造型铅锌矿床。
        Deke lead-zinc deposit is an important lead-zinc deposit discovered in Xinjiang. It distributes in Aktao County, Xinjiang. The main mineralization is lead-zinc deposit. The deposit occurs in a set of carbonate-clastic formation strata of shallow metamorphic marine or marine-continental alternating facies deposited in the Middle-Upper Paleozoic depression. The ore structure is simple, mainly irregular granular and schist, and the ore structure is disseminated. Shape and vein. Based on the analysis of geochemical characteristics of the deposit, the genesis of the deposit is discussed. It is considered that the genesis of the deposit belongs to stratabound hydrothermal reformed lead-zinc deposit.

引文

[1]杨向荣.新疆塔木铅锌矿成矿流体特征与矿床成因[J].地质勘探工程学院，2016,(02).
    [2]刘焱.新疆塔木铅锌矿成矿流体特征与矿床成因[J].新疆勘探工程学院，2017(10).