若羌库木苏铜矿地质特征及成因初探
Geological Characteristics and Genesis Analysis of Kumusu Copper Deposit in Ruoqiang County,Xinjisng
付清波 1刘兵 1罗耀鸿 1李月栋 1胡力升1
作者信息
- 1. 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
- 折叠
摘要
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.
Abstract
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.
关键词
库木苏/铜矿/辉长岩/成因分析Key words
Kumusu/Copper deposit/Gabbro/Cause-effect analysis引用本文复制引用
基金项目
新疆若羌县库木苏一带金铜多金属矿调查评价(K14-2-LQ06)
出版年
2024
NETL
NSTL
万方数据