摘要
通过对西准包古图地区铜金矿床(点)地质特征分析,认为该区铜金矿属与中酸性小岩体有关的铜金矿成矿系列,自岩体至围岩岩石蚀变、矿床类型、成矿元素组合均具一定的分带性,对该区铜金矿的成矿规律和成矿机制进行了初步探讨,在此基础上指出了该区进一步的找矿方向。
Based on geological characteristics of Cu - Au deposits in the Baogutu area, western Jungar Basin, it is concluded that Cu - Au mineraliza- tion is related with the small intermediate - acid intrusive bodies. Wallrock alteration, mineralizing style, and mineralization element association show certain zonation from intrusive bodies to wallrocks. On the base of discussion of the mineralization regularity and mechanism, prospecting direction in the area is proposed.
出处
《地质与勘探》
CAS
CSCD
北大核心
2006年第4期11-15,共5页
Geology and Exploration
基金
新疆地质勘查中央专项资金项目(编号:200342002035)资助
关键词
新疆
包古图
铜金矿
成矿规律
成矿机制
Xinjiang, Baogutu,Cu -Au deposit,mineralization regularity,mineralization mechanism
