内蒙古科尔沁右翼前旗复兴屯2区银铅锌矿地质特征及找矿标志  

Geological characteristics and prospecting criteria of the No.2 mining area of Fuxingtun Ag-Pb-Zn deposit in the Horqin Right Front Banner,Inner Mongolia

作　　者：樊树启 刘俊杰 徐同宝 梁新强 李敏[2] 李海军[2] FAN Shuqi;LIU Junjie;XU Tongbao;LIANG Xinqiang;LI Min;LI Haijun(Geological Exploration Fund Management Center of Inner Mongolia Autonomous Region,Hohhot 010020,China;Inner Mongolia Land Resources Exploration and Development Co.,Ltd.,Hohhot 010020,China)

机构地区：[1]内蒙古自治区地质勘查基金管理中心,呼和浩特010020 [2]内蒙古国土资源勘查开发有限责任公司,呼和浩特010020

出　　处：《有色金属（矿山部分）》2021年第1期75-80,共6页NONFERROUS METALS(Mining Section）

基　　金：内蒙古自治区地质勘查基金项目(11-1-KC11)。

摘　　要：复兴屯2区银铅锌矿位于内蒙古自治区科尔沁右翼前旗,属突泉—翁牛特Pb、Zn、Cu、Mo、Au成矿带,矿体呈近东西走向主要赋存于中酸性火山碎屑岩中,矿区共圈定3个矿段,82条矿体,矿体主要呈脉状、透镜状。矿床成因类型为受火山构造控制的火山-次火山热液充填型。通过深入研究该矿床区域成矿构造地质背景和区内成矿地质条件,总结主要矿体特征,进而浅析了矿床成因及找矿标志。The second mining area of Fuxingtun Ag-Pb-Zn deposit,located in the Horqin Right Front Banner of Inner Mongolia,belongs to the Tuquan-Wengniute banner Pb,Zn,Cu,Mo,and Au metallogenic belt.There are three ore sections and 82 ore bodies in the mining area,and the ore bodies are mainly veined and lenticular.The deposit is a volcanic-subvolcanic hydrothermal filling type,controlled by volcanic structure.In this paper,the geotectonic background and metallogenic geological conditions of the deposit were studied,the characteristics of main ore bodies were summarized,and the genesis and prospecting criteria of the deposit were analyzed.

关 键 词：银铅锌矿 地质特征 找矿标志 科尔沁右翼前旗 复兴屯2区 

分 类 号：P62[天文地球—地质矿产勘探]