四川丹巴磨子沟金矿成矿模式浅析  

The Metallogenic Model of Mozigou Gold Desposit in Sichuan Danba Areas

作　　者：熊发挥[1] 肖渊甫[1] 黄耀宗[1] 冯伟[1] 牛刚[1] 康从轩[1] 

机构地区：[1]成都理工大学,成都610059

出　　处：《四川有色金属》2009年第2期9-11,共3页Sichuan Nonferrous Metals

摘　　要：四川西部丹巴地区的地质构造总体以背斜为主,区内顺层韧性剪切高应带及破碎带发育,并大量出露矿化石英脉。矿区岩性主要是深灰色、灰色炭质板岩、页岩、千枚岩、片岩组成的复理式建造,赋矿岩石、矿化形成、矿物组合、及元素组成,均可与穆龙套型金矿床进行对比,具有了穆龙套金矿典型地质特征。Danba areas of western Sichuan general geological structure to the main anticline, bedding area should be ductile shear zones and high fracture zone development, and a large number of exposed quartz vein mineralization. Mining lithology is dark gray, carbonaceous slate, shale, phyllite, schist, composed of Flysch-type construction, ore rocks, the formation of mineralization, mineral composition, Muruntau dwelling size and can be compared with gold deposits, with the typical gold Muruntau geological features.

关 键 词：金矿 地质特征 穆龙套 

分 类 号：P618.51[天文地球—矿床学] P618.130.2[天文地球—地质学]