摘要
新疆布尔克斯岱金矿床产于下石炭统黑山头组细碎屑岩中 ,矿体产出受EW向断裂构造控制。矿石类型主要为构造蚀变岩型。EH4连续电导率测量表明 ,该矿床深部存在明显的地球物理异常 ,异常长度大于 90 0m ,宽度大于 10m ,延伸大于 10 0 0m ,展示了金矿床深部具有良好的成矿前景 ,是一个有利的大型金矿找矿靶区。
The Buerkesidai gold deposit occurs within lower Carboniferous carbon-bearing rocks. The ore bodies are controlled by E-W strike fault structure. The ore types are mainly structural altered rock type. The results of EH4 Electrical Conductivity Imaging system measurement show that there is a clear geophysical anomaly in depth of the Buerkesidai deposit. The anomaly exceeds 900m in length,10m in width and 1000m in depth. It is indicated that the Buerkesidai gold deposit has a good metallogenic prospects and might become a big type exploration target for gold.
出处
《地质与勘探》
CAS
CSCD
北大核心
2004年第4期17-20,共4页
Geology and Exploration
基金
国家"十五"科技攻关项目 (编号 :2 0 0 1BA60 9A -0 7-0 8)
中国科学院创新工程项目 (编号 :KZCX3 -SW -13 7)资助
