曹强, 刘家军, 吴杰, 陶银龙, 王立新, 刘相红. 秦岭西部铧厂沟金矿床主矿带原生晕分带特征及深部预测[J]. 地质与资源, 2021, 30(1): 27-36, 98. DOI: 10.13686/j.cnki.dzyzy.2021.01.004
    引用本文: 曹强, 刘家军, 吴杰, 陶银龙, 王立新, 刘相红. 秦岭西部铧厂沟金矿床主矿带原生晕分带特征及深部预测[J]. 地质与资源, 2021, 30(1): 27-36, 98. DOI: 10.13686/j.cnki.dzyzy.2021.01.004
    CAO Qiang, LIU Jia-jun, WU Jie, TAO Yin-long, WANG Li-xin, LIU Xiang-hong. PRIMARY HALO ZONING AND DEEP PREDICTION OF THE MAIN ORE BELT IN HUACHANGGOU GOLD DEPOSIT, WESTERN QINLING MOUNTAINS[J]. Geology and Resources, 2021, 30(1): 27-36, 98. DOI: 10.13686/j.cnki.dzyzy.2021.01.004
    Citation: CAO Qiang, LIU Jia-jun, WU Jie, TAO Yin-long, WANG Li-xin, LIU Xiang-hong. PRIMARY HALO ZONING AND DEEP PREDICTION OF THE MAIN ORE BELT IN HUACHANGGOU GOLD DEPOSIT, WESTERN QINLING MOUNTAINS[J]. Geology and Resources, 2021, 30(1): 27-36, 98. DOI: 10.13686/j.cnki.dzyzy.2021.01.004

    秦岭西部铧厂沟金矿床主矿带原生晕分带特征及深部预测

    PRIMARY HALO ZONING AND DEEP PREDICTION OF THE MAIN ORE BELT IN HUACHANGGOU GOLD DEPOSIT, WESTERN QINLING MOUNTAINS

    • 摘要: 为了解铧厂沟金矿原生晕分布规律、提高找矿勘查效率,对铧厂沟金矿的原生晕进行了元素相关性分析、R型聚类分析以及因子分析等,并结合了野外工作及前人研究成果,得到铧厂沟金矿床理想的分带组合:前缘晕为As-Te-Sb-Hg,近矿晕为Ag-Au-Bi-Pb-Zn-Se,尾晕为Sc-Co-Ni-Mo-Cu-Cd-Mn.铧厂沟金矿的主矿带分带顺序为:Sc-Se-Mn-Cu-Cd-Ni-Zn-Ag-Au-Pb-Sb-Mo-Te-Co-Bi-Hg.结合原生晕理想的叠加模型,得到矿体从1150中段至990中段呈现不连续现象,表现为在1070中段以及下部矿体延伸至1030中段附近出现尖灭.新矿体从1030中段再次出现往下部延伸至990中段附近,并且存在往深部延伸的趋势.

       

      Abstract: To know about the distribution rule of primary halo in Huachanggou gold deposit and improve the efficiency of prospecting and exploration, the paper makes the element correlation analysis, R-mode cluster analysis and factor analysis of the primary halo, combined with the field survey and previous research results, and obtains the ideal zoning combination of Huachanggou gold deposit as follows: As-Te-Sb-Hg for the front halo, Ag-Au-Bi-Pb-Zn-Se for the near-ore halo and Sc-Co-Ni-Mo-Cu-Cd-Mn for the rear halo, with Sc-Se-Mn-Cu-Cd-Ni-Zn-Ag-Au-Pb-Sb-Mo-Te-Co-Bi-Hg as the zoning sequence of main ore belt. Combined with the ideal model of primary superimposed halo, it is concluded that the orebody is discontinuous from Level 1150 m to Level 990 m, that is, the orebody extending from Level 1070 m downward and pinching out near Level 1030 m, then appearing again from Level 1030 m to Level 990 m, showing a tendency of deep extension.

       

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