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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
闫庆贺; 王核; 丘增旺; 魏小鹏; 李沛
Source Publication中国矿物岩石地球化学学会第九次全国会员代表大会暨第16届学术年会文集
2017-04-18
Conference Date2017-04-18
Conference Place中国陕西西安
Country中国
Indexed By其他
Language中文
Keyword大红柳滩 矿物 伟晶岩矿床 内生矿床 铌钽铁矿 锡石 锡矿物 西昆仑
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)矿床及牧林
Document Type会议论文
Identifierhttp://ir.gig.ac.cn/handle/344008/35548
Collection中国科学院矿物学与成矿学重点实验室_会议论文
Recommended Citation
GB/T 7714
闫庆贺,王核,丘增旺,等. 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[C],2017.
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