摘要
曼家寨西矿段多金属矿床属层控矽卡岩型。锡锌矿受地层、岩相、变质带、构造及隐伏花岗岩体等综合地质因素控制。由多期成矿作用、多来源物质、多成因成矿热液反复活化、迁移、聚集、分配和沉淀形成。
The muhimetallic deposit of W Manjiazhai ore block belongs to the stratabound skarn type. The Sn- Zn ore body is controlled by the comprehensive geological factors of strata, lithofacies, metamorphic zone, structure and buried granite body, etc. It is formed because of repeated activization, migration, accumulation, distribution and settlement of muhiphase metallogenesis, material source and polygenetic metallogenetic thermal fluid.
出处
《云南地质》
2013年第3期296-299,共4页
Yunnan Geology
关键词
矽卡岩型
多金属锡锌矿床
多期多源多成因
硅酸盐类矿石
云南都龙曼家寨
Skarn Type
Multimetallic Sn - Zn Deposit
Muhiphase, Multiple source, Multigenetic
Silicate Ore
Manjiazhai, Dulong, Yunnan
