东昆仑西段巴什尔希花岗岩与白干湖钨锡矿床的关系  

Relations between Bashenerxi granite,west Dongkunlun and Baiganhu tungsten-tin deposit

作　　者：包亚范 刘延军[1] 王鑫春[1] 

机构地区：[1]吉林省第三地质调查所,吉林四平136000

出　　处：《吉林地质》2008年第3期56-59,67,共5页Jilin Geology

摘　　要：自2001年吉林省地质调查院在东昆仑西段发现白干湖钨、锡矿床后,国家地质调查局在该区外围相继布置了大面积的1/5万矿产远景调查项目。据区域地质调查资料并结合白干湖钨、锡矿床勘查成果资料分析,白干湖一带钨锡矿产的成矿作用与巴什尔希二长花岗岩关系密切。The tungsten-tin deposit was discovered in west Dongkunlun area since 2001,Bureau of National Geologic Survey has arranged 1∶50 000 mineral long-range investigations in succession in the outer area of the study area.Through the regional geologic investigation data and tungsten-tin deposit exploration data,it is considered that ore-forming process of the Baiganhu tungsten-tin deposit is closely related with the Bashenerxi adamellite.

关 键 词：东昆仑西段 白干湖钨锡矿床 巴什尔希二长花岗岩 “S”型花岗岩 

分 类 号：P618.44[天文地球—矿床学]