内蒙古阿巴嘎旗某萤石矿矿床成因与找矿思路  

Genesis and Prospecting Ideas of A Fluorite Ore Deposit in Abagaqi,Inner Mongolia

作　　者：刘亭[1] 齐艳妮[1] 牟业龙[1] 张峰 LIU Ting;QI Yan-ni;MU Ye-long;ZHANG Feng(Northwest Research Institute of Mining and Metallurgy,Baiyin 730900,China)

机构地区：[1]西北矿冶研究院,甘肃白银730900

出　　处：《甘肃冶金》2021年第3期111-113,共3页Gansu Metallurgy

摘　　要：通过对区域成矿地质背景、矿床地质特征、控矿构造及成矿规律进行分析研究,认为本区萤石矿成因为中-低温热液充填交代型脉状萤石矿床,下一步地质找矿应围绕燕山期花岗岩发育区域,在断裂构造破碎带发育且宽大的区域、硅化强烈的部位寻求找矿突破。This article through to the regional metallogenic geological setting,geological features,ore-controlling tectonic and metallogenic regularity analysis,think in fluorite ore into because of low temperature hydrothermal filling metasomatic type vein fluorite ore deposit,geological prospecting should be around next yanshanian granite development area,the fault fracture zone development and the wide area,silicide strong area for prospecting breakthrough.

关 键 词：内蒙古 萤石矿 地质特征 矿床成因 

分 类 号：P619.215[天文地球—矿床学]