吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (1): 70-84.doi: 10.13278/j.cnki.jjuese.20180218
• 地质与资源 • 上一篇
林成贵1,2, 程志中1,2, 吕志成1,2, 颜廷杰1,2, 贾儒雅1,2, 姚晓峰1,2, 宓奎峰1,2, 李康宁3
Lin Chenggui1,2, Cheng Zhizhong1,2, Lü Zhicheng1,2, Yan Tingjie1,2, Jia Ruya1,2, Yao Xiaofeng1,2, Mi Kuifeng1,2, Li Kangning3
摘要: 甘肃省早子沟金矿位于西秦岭西段,是20世纪末通过1:20万化探扫面发现的超大型金矿,该矿床是典型的中低温岩浆热液矿床,矿体主要受断裂构造和脉岩的控制。为了解决深部找矿的问题,本文收集了矿区61个钻孔相关资料,得到了4 012个钻孔原生晕的数据。通过对原生晕数据进行相关性分析、R型聚类分析、因子分析和原生晕浓度分带特征研究,认为找矿的最佳指示元素为Au、As、Sb、Ag、Hg、W,其中与Au成矿最密切、最直接的指示元素是As和Sb;通过计算原生晕分带指数,得到了原生晕轴向分带序列(从上到下)为Au-Hg-Bi-Pb-Mo-Sb-Ag-Cu-W-Zn-Co-As,Sb和As等前缘指示元素出现在尾晕元素之后,显示深部可能存在盲矿体。基于以上研究,结合地质方面的认识,评价了矿区深部含矿性,提取了深部找矿信息。并据此构建了早子沟金矿地质-地球化学深部找矿模型,圈出了2处深部找矿靶区。
中图分类号:
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