易门县狮子山铜矿成矿地质条件及深部找矿前景  

THE METALLOGENETIC GEOLOGICAL CONDITIONS AND DEEP PROSPECTING POTENTIALITY OF SHIZISHAN CU DEPOSIT,YIMEN

作　　者：毛建辉[1] 郭祖江 潘庆周 

机构地区：[1]玉溪矿业有限公司,云南玉溪653100

出　　处：《云南地质》2015年第1期67-70,共4页Yunnan Geology

摘　　要：易门狮子山铜矿为沉积-改造型铜矿。受地层、岩性和构造的控制,层状矿体产于狮子山倒转背斜北西翼中元古界昆阳群落雪组白云岩中,柱状矿体分布于褶皱转折端落雪组白云中,成矿条件优越,深部有一定找矿潜力。Shizishan Cu deposit in Yimen is a sedimentation-reformation Cu deposit, controlled by the strata, lithological character and structure. The bedded ore is in Middle Proterozoic Luoxue Formation dolomitite on the NW limb of Shizishan reversed fold, whereas the column ore body is in Luoxue Formation dolomitite on the fold turning end. The metallogenesis conditions are excellent, with a certain prospecting potentiality in the deep.

关 键 词：沉积改造型铜矿 地层—构造控矿 云南易门狮子山 

分 类 号：P618.41[天文地球—矿床学]