新平大红山铜铁矿床控矿因素及成因分析  

AN ANALYSIS OF ORE CONTROL FACTOR & GENESIS OF DAHONGSHAN CU-FE DEPOSIT,XINPING

作　　者：宁佐金 

机构地区：[1]玉溪矿业有限公司大红山铜矿,云南玉溪新平653400

出　　处：《云南地质》2010年第4期409-415,381,共8页Yunnan Geology

摘　　要：大红山铜铁矿床是我国著名的大型铁铜矿床之一。对成矿地质背景、矿床地质、矿体特征等综合研究,分析矿床控矿因素,提出矿床成因为火山-喷发沉积变质型,建立了成矿模式。The Dahongshan Cu - Fe deposit is one of the most famous large Fe - Cu deposit in China. According to the comprehensive study on geological background of metallogenesis, geology of ore deposit, characteristics of ore body, we have an analysis of the ore control factor of ore deposit and put forward that the genesis of ore deposit is the type of volcanic eruption deposition metamorphism and then establish the metallogenetic model.

关 键 词：沉积变质型 控矿因素 矿床地质 大红山铜铁矿 云南新平 

分 类 号：P618.41[天文地球—矿床学]