摘要
邱村金矿床为受断裂破碎带控制的陆相火山岩中—低温热液型金矿床,矿体产于燕山中期南园组(J_3n^2)和长林组(J_3c)地层中。通过综合分析该矿区成矿地质背景、矿体地质特征、矿床控矿因素以及找矿标志,并对区内找矿方向进行讨论,为区内找矿工作提供参考。
Qiucun gold deposit is belongs to the continental volcanic rock medium-low temperature hydrothermal type gold deposit that is controlled by fault fracture zones,the orebody of Qiucun gold deposit originated in the strata of middle Yanshan garden group( J_3n^2) and Changlin group( J_3c). Based on analyzing the ore-forming geological background,geological characteristics of the mining area,the orecontrolling factors and prospecting indicators of Qiucun gold deposit are discussed in depth,besides that,the prospecting direction of the mining area is also researched to provide reference for the prospecting work in the mining area.
出处
《现代矿业》
CAS
2015年第12期84-86,共3页
Modern Mining
关键词
地质特征
控矿因素
找矿标志
找矿方向
金矿
Geological characteristics
Ore-controlling factors
Prospecting indicators
Prospecting direction
Gold mine