摘要
何宝山金矿床具有构造破碎带蚀变岩型金矿床的重要特征。断裂构造对金矿化具有严格的控制作用。文章主要介绍桂林矿产地质研究院在矿区开展的地质、物探、化探综合找矿预测研究工作,通过对该矿床进行成矿地质条件分析、物探电法测量以及化探新方法测量,对何宝山金矿床深部及外围的成矿潜力进行了综合评价,为矿区下一步的找矿工作指明了方向。
Hebaoshan gold deposit belongs to a typical structural alteration rock type deposit. Gold mineralization is definitely controlled by fault structures. Geological, geophysical and geochemical exploration and prediction history by Guilin Institute of Geology for Mineral Resources is introduced. Based on geological mineralization conditions, geophysical electric measurement and new geochemical results, mineralizing potential in the deep and periphery of Hebaoshan gold deposit are synthetically evaluated. The prospecting targets are pointed out for future exploration work.
出处
《地质与勘探》
CAS
CSCD
北大核心
2007年第6期70-75,共6页
Geology and Exploration
基金
广西科学基金项目(桂科回0448023)资助。
关键词
何宝山金矿
成矿地质条件
物探电法
化探新方法
找矿预测
Hebaoshan gold deposit, geological mineralization condition, geophysical electric method, new geochemical method, exploration and prospecting
