内蒙古巴根黑格其尔铅锌矿地质特征及找矿研究  

GEOLOGICAL CHARACTERISTICS AND PROSPECTING RESEARCH OF BAGENHEIGEQIER LEAD-ZINC DEPOSIT IN INNER MONGOLIA

作　　者：王保国 杨钦淞 WANG Bao-guo;YANG Qin-song(Chengtun Mining Group Co.,LTD,Xiamen 361100,Fujian;Yunnan Geological Engineering Survey and Design Research Institute Co.,Ltd,Kunming 650041)

机构地区：[1]盛屯矿业集团股份有限公司,福建厦门361100 [2]云南地质工程勘察设计研究院有限公司,云南昆明650041

出　　处：《云南地质》2024年第1期26-30,共5页Yunnan Geology

摘　　要：内蒙古巴根黑格其尔铅锌矿床赋存于上石炭统宝力格庙组安山质凝灰岩中,呈透镜状、脉状。F 3断层是重要的控矿构造,二长花岗斑岩床对成矿控制作用明显,高磁异常对找矿具有直接的指示作用。本文在总结矿床地质特征、矿床成因、成矿规律及控矿因素等基础上,以地层、构造、岩浆岩、成矿空间、磁异常“五位一体”找矿模式选出两处靶区,以期实现找矿突破,为矿区增储上产提供资源基础。The Bagenheigeqier lead-zinc deposit in Inner Mongolia occurs in the andesitic tuff of the Upper Carboniferous Baoligemiao Formation,which is lenticular and veined.The F3 fault is an important ore-controlling structure.The monzonitic granite porphyry has obvious ore-controlling effect on mineralization,and the high magnetic anomaly has a direct indication for prospecting.Based on summarizing the geological characteristics,genesis,metallogenic regularity and ore-controlling factors of the deposit,two target areas were selected by the'five in one prospecting model of strata,structure,magmatic rock,metallogenic space and magnetic anomaly,in order to achieve a breakthrough in prospecting.

关 键 词：岩性+构造 五位一体 找矿模式 找矿方向 巴根黑格其尔铅锌矿 内蒙古 

分 类 号：P618.42[天文地球—矿床学] P43[天文地球—地质学]