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若羌库木苏铜矿地质特征及成因初探

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库木苏铜矿产于红柳沟-喀腊大湾裂谷带东部卓阿布拉克杂岩体中,为近年来在阿尔金东段奥陶纪辉长岩建造内发现的铜矿产地.通过对库木苏铜矿区成矿地质背景、化探异常、蚀变带及矿体特征的研究,分析成矿环境和控矿因素,初步认为该矿属岩浆硫化物型铜矿床,具良好的找矿潜力.
Geological Characteristics and Genesis Analysis of Kumusu Copper Deposit in Ruoqiang County,Xinjisng
The Kumusu copper deposit is located in the Zhuobulake complex in the eastern part of the Hongliugou-Ka-ladawan Rift Zone.It is a copper deposit discovered in recent years within the Ordovician gabbro formation in the east-ern section of Arkin.Based on geological data obtained from field exploration,this article analyzes the ore-forming geo-logical background,geochemical anomalies,alteration zones,and ore body characteristics of the mining area,analyzes the ore-forming environment and controlling factors,and preliminarily believes that the deposit belongs to the magmatic sulfide type copper deposit with good prospecting potential.

KumusuCopper depositGabbroCause-effect analysis

付清波、刘兵、罗耀鸿、李月栋、胡力升

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新疆维吾尔自治区地质矿产勘查开发局第一区域地质调查大队,新疆乌鲁木齐 830011

库木苏 铜矿 辉长岩 成因分析

新疆若羌县库木苏一带金铜多金属矿调查评价

K14-2-LQ06

2024

新疆地质
新疆维吾尔自治区地质学会

新疆地质

CSTPCD
影响因子:0.879
ISSN:1000-8845
年,卷(期):2024.42(2)