摘要
位于东天山东段的台曼苏泉金矿产于层间蚀变破碎带内,矿体严格受破碎带所控制,构造控矿特征明显。本文从地球化学特征方面入手着重对地表地球化学特征以及深部垂向地球化学分带特征进行阐述,并以此为基础对该矿的找矿前景作了分析,明确了该区下一步找矿方向。
The Taimansuquan gold deposit in the Eastern Tianshan is hosted in the interformational altered fracture zone, and the ore bodies are mainly controlled by these faults with clearly structural ore-control characteristics. This paper reports the geochemical characteristics of the surface and shows the vertical geochemical zoning for the lower part of the deposit. Based on these data, we analysis the metallogenic potential and point out the prospecting direction of the Taimansuquan gold deposit.
出处
《甘肃冶金》
2016年第3期95-97,102,共4页
Gansu Metallurgy
关键词
地球化学特征
金矿
台曼苏泉
找矿前景
钻孔原生晕
geochemical characteristics
gold deposit
Taimansuquan
prospecting potential
primary halo of drill hole
