新疆伊宁县塔乌尔别克金矿地质特征及成因分析  

Geological characteristics and genetic analysis of Tawuerbieke gold deposit in Yining County,Xinjiang

作　　者：何英[1] 邹存海 张江[1] 

机构地区：[1]中国冶金地质总局新疆地质勘查院,乌鲁木齐830063

出　　处：《地质找矿论丛》2015年第2期221-227,共7页Contributions to Geology and Mineral Resources Research

摘　　要：塔乌尔别克金矿是西天山吐拉苏断陷盆地火山岩带浅成低温热液型金矿集中区的一个金矿床,矿体主要赋存于下石炭统大哈拉军山组地层中。文章阐述了塔乌尔别克金矿床地质特征,探讨了矿床成因,认为塔乌尔别克金矿属于火山-次火山浅成低温热液型金矿床。fault basin Formation. considered Tawuerbieke gold deposit is one of the epithermal Au deposits of volcanic rock belt in Tulasu in the west Tianshan area. Ore bodies occur mainly in the Lower Carboniferous Dahalajunshan This paper describes geological characteristics and discusses genesis of the deposit and it is a volcanic-sub-volcanic epithermal gold deposit.

关 键 词：塔乌尔别克金矿 火山-次火山浅成低温热液矿床 地质特征 成因分析 新疆 

分 类 号：P613[天文地球—矿床学] P618.51[天文地球—地质学]