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.
出处
《云南地质》
2010年第4期409-415,381,共8页
Yunnan Geology
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
Deposition - Metamorphism Type
Factor of Ore Control
Geology of Ore Deposit
Dahongs- han Cu-Fe Deposit
Xinping, Yunnan
