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西昆仑大红柳滩稀有金属伟晶岩矿床锡石及铌钽铁矿年代学及其地质意义
Authors
丘增旺
李沛
+3 more
王核
闫庆贺
魏小鹏
Publication date
18 April 2017
Publisher
Abstract
西昆仑造山带由北向南可分为塔里木板块、奥依塔格-库地-苏巴什缝合带、西昆仑地体、麻扎-康西瓦缝合带、甜水海地体、红山湖-乔尔天山缝合带和羌塘板块(潘裕生和王毅,1994;Xiao等,2000)。本地区花岗伟晶岩相当发育,区内主要分布有木吉-布伦口矿田、班迪-五其矿田、三素-维布隆矿田、康西瓦-大红柳滩矿田4个矿田,构成了新疆重要的伟晶岩成矿带。其中大红柳滩锂铍(铌钽)矿床及牧
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Last time updated on 27/11/2019