云南禄劝付腥田铁矿地质特征  

THE GEOLOGICAL FEATURE OF FUXINGTIAN FE DEPOSIT IN LUQUAN,YUNNAN

作　　者：高蕊 宋晟 

机构地区：[1]云南贵宝地质勘察设计有限公司,云南昆明650093

出　　处：《云南地质》2014年第3期346-350,共5页Yunnan Geology

摘　　要：通过对云南禄劝付腥田铁矿区的地质普查工作,发现了2个赤铁矿体、2个磁铁矿体和3个铁矿化点,铁矿体受控于中元古界美党组五段、三段,矿床成因为美党组高含铁质碎屑沉积再经后期热液改造的沉积变质型铁矿床。According to the geological prospecting in Luquan Fuxingtian Fe orefield, we have discovered 2 hematite bodies, 2 magnetite bodies and 3 Fe metallogenesis spots. The Fe ore bodies are controlled by Middle Proterozoic Meidang Formation Member 3, 5. It is a sedimentary metamorphic type Fe deposit formed by Meigang Formation high Fe-bearing elastic sediment and the later hydrothermal reformation.

关 键 词：铁质沉积 热液蚀变 层状矿床 云南禄劝付腥田 

分 类 号：P618.31[天文地球—矿床学]