内蒙古自治区东乌旗朝不楞矿区铁锌多金属矿床控矿因素及成因分析  

Analysis on the ore controlling factors in chaobuleng Fe Zn polymetallic deposit and genesis of the Inner Mongolia Autonomous Region Dongwuqi

作　　者：周光泽 

机构地区：[1]成都理工大学,四川成都610059

出　　处：《世界有色金属》2017年第14期180-181,共2页World Nonferrous Metals

摘　　要：朝不楞多金属矿区位于内蒙古自治区东乌珠穆沁旗东北部,本论文在区域成矿地质背景分析的基础上,系统总结了矿床地质特征。据收集到的资料和前人研究成果,分析了成矿物理化学条件,总结了成矿流体的性质和特征,得出了矿床成矿物质、热液的来源和矿床成因的初步结论。Chaobuleng polymetallic deposit is located in the northeast of Dong Ujimqin banner in Inner Mongolia Autonomous Region, based on the regional geological background analysis, summarizes the geological characteristics of the deposit. According to the collected data and the results of previous studies, analysis of the physical and chemical conditions of mineralization, summed up the nature and characteristics of ore-forming fluids, and draws the preliminary conclusion of metallogenic material, hydrothermal source and genesis of the deposit.

关 键 词：铁锌多金属矿 控矿因素 成因分析 

分 类 号：P618.41[天文地球—矿床学]