内蒙古突泉县闹牛山铜矿地质特征及找矿标志  

Geological Characteristics and Prospecting Indicators of Naoniushan Copper Deposit in Tuquan County,InnerMongolia

作　　者：孟宪林 林小磊 MENG XIAN-lin;LIN Xiao-lei(Beijing Huaxia Jianlong Mining Technology Co.,Ltd.,Beijing 10000,China;The No.514 Geological Brigade of North China Geological Survey Bureau,Chengde Hebei 067000,China)

机构地区：[1]北京华夏建龙矿业科技有限公司,北京100000 [2]华北地质勘查局五一四地质大队,河北承德067000

出　　处：《西部探矿工程》2024年第12期82-85,88,共5页West-China Exploration Engineering

摘　　要：内蒙古突泉县闹牛山铜矿的矿床构造属于大陆边缘裂陷带的局部隆起部分,它位于大兴安岭火山带的中段,矿地质条件十分有利,具有非常好的找矿前景。通过矿区地质特征研究,对闹牛山铜矿成矿的地质背景进行分析,总结了控矿因素及矿床成因,获得了较好的找矿信息,并提出了成矿远景及找矿方向,为该地区下一步勘查工作提供了依据。The Naoniushan copper deposit in Tuquan County,Inner Mongolia,belongs to the locally uplifted part of the continental margin rift zone and is located in the middle section of the Daxing'anling volcanic belt.The geological conditions for mineralization are very favorable and have very good prospects for mineral exploration.This article analyzes the geological background of the mineralization of the Naoniushan copper mine through the study of the geological characteristics of the mining area,summarizes the controlling factors and genesis of the deposit,obtains good prospecting information,and proposes mineralization prospects and prospecting directions,providing a basis for the next exploration work in the area.

关 键 词：地质特征 找矿方向 铜多金属 内蒙古突泉 

分 类 号：P618.41[天文地球—矿床学]