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    电极电位测井在低品位金矿勘查中的应用研究——以宝兴沟金矿为例

    Application of electrode potential logging in the exploration of low-grade type gold deposits: A case study of the Baoxinggou gold deposit

    • 摘要:
      研究目的 针对低品位浸染状金矿地球物理信号弱、信噪比低、勘探难度大的问题,本文旨在通过精细识别有利成矿层,为金矿勘查提供有效方法支撑。宝兴沟金矿是一座典型的浸染状中低温热液型大型金矿,平均品位1.43×10−6,赋存于中侏罗统二十二站组碎屑砂岩中。本文以宝兴沟金矿为例,重点研究如何利用地球物理测井手段,建立适用于该类矿床的有利成矿层识别标志。
      研究方法 在宝兴沟金矿区2个钻孔中系统开展地球物理多参数测井工作,结合钻孔岩心编录与样品分析数据,对比分析不同金富集程度的测井响应特征。通过定量分析金品位与电极电位异常幅值之间的相关关系,建立基于电极电位测井的有利成矿层识别标志。
      研究结果 具有金属矿化或强烈蚀变的地层在电极电位测井曲线上表现为锯齿状异常,其中多峰高值异常段对应浸染状矿体的有利成矿层。金相对富集区的电极电位曲线呈密集脉冲型或单个宽幅型异常,而贫瘠区则表现为稀疏尖脉冲型异常。
      结论 基于电极电位测井建立的有利成矿层识别标志,能够有效圈定赋金有利层位,实现浅表区域的精细找矿,并为钻探工程部署提供可靠依据。该研究成果不仅适用于浅部矿化识别,也为深部找矿工作提供了方法借鉴与实践参考。

       

      Abstract:
      This paper is the result of mineral exploration engineering.
      Objectives Aimed at addressing the challenges of weak geophysical signals, low signal-to-noise ratio, and high exploration difficulty in low-grade gold deposits, this study focuses on the precise identification of favorable mineralization horizons to provide an effective methodological support for gold exploration. The Baoxinggou gold deposit is a typical large-scale disseminated epithermal gold deposit, with an average grade of 1.43 ppm. It is hosted within the clastic sandstones of the Middle Jurassic Ershierzhan Formation. Taking the Baoxinggou gold deposit as an example, it investigates how to utilize geophysical logging techniques to establish identification criteria for favorable mineralization horizons applicable to this type of deposit.
      Methods Systematic multi-parameter geophysical logging was conducted in two boreholes within the Baoxinggou gold mining area. By integrating data from drill core logging and sample analysis, the logging response characteristics corresponding to different gold enrichment levels were compared and analyzed. Through quantitative analysis of the correlation between gold grade and the amplitude of electrode potential anomalies, identification criteria for favorable mineralization horizons based on electrode potential logging were established.
      Results The strata exhibiting metallic mineralization or intense alteration display serrated anomalies in electrode potential logging curves. Within these anomalies, multi-peak high-amplitude segments correspond to favorable mineralization horizons of disseminated ore bodies. In gold-enriched zones, the electrode potential curves exhibit intensive pulse-shaped or individual broad-amplitude anomalies, whereas barren zones are characterized by sparse sharp pulse-shaped anomalies.
      Conclusions The identification criteria for favorable mineralization horizons established based on electrode potential logging can effectively delineate gold-bearing layers, enabling precise near-surface prospecting and providing a reliable basis for drilling program design. This research not only applies to shallow mineralization identification but also offers methodological guidance and practical reference for deep mineral exploration.

       

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