摘要
本文在野外补充勘查工作及室内综合研究整理的基础上,总结了刘家金矿床的成矿地质背景、矿床地质,认为矿体主要赋存于铁砂街群中元组变凝灰岩顺层破碎带中,受NNE向F6断层控制,成矿与闪长岩密切相关。同时指出了矿区今后找矿方向,认为深边部找矿潜力大。
In this paper, the exploration in the field of comprehensive research work and interior finishing on the basis of summing up the metallogenic geological background, ore deposit geology Liu gold deposit, that the ore bodies mainly occur in the tieshajie group of tuples in the tuff bedding fracture zone, controlled by the NNE to the F6 fault, the mineralization is closely related to diorite. At the same time, the prospecting direction in the mining area is pointed out in the future, and it is considered that the prospecting potential of the deep edge is great.
出处
《世界有色金属》
2017年第22期80-81,共2页
World Nonferrous Metals
关键词
矿床地质特征
找矿方向
变凝灰岩
闪长岩
弋阳刘家
geological features of ore deposits
prospecting direction
variable tuff
diorite
Yiyang Liu's family