岩心磁化率数据在找矿勘查工作中的应用分析
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中国地质调查局牡丹江自然资源综合调查中心

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Application Analysis of Core Magnetic Susceptibility Data in Mineral Exploration
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Mudanjiang Comprehensive Natural Resources Survey Center, China Geological Survey

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    摘要:

    本研究以松江河金矿外围找矿勘查工作区为例,通过对3个钻孔岩心的磁化率测量及对比分析,探讨了岩心磁化率数据在找矿勘查中的应用效果。研究采用加拿大KT-10型便携式磁化率仪,测量了1858个岩心样品,结合钻孔柱状图与磁化率曲线对比分析,研究结果表明:岩心磁化率数据对黄铁矿化位置的标记作用显著,能够有效指示矿化蚀变带;磁化率参数在地层划分中具有辅助作用,有助于区分不同岩性及构造特征。具体定量结果如下:钻孔ZK1岩心磁化率数据最大值为147.727×10?3(SI),最小值为0.013×10?3(SI),平均值为2.82482×10?3(SI)。在矿化蚀变强烈的区段(如49.00 - 50.00m、65.50 - 67.50m等),磁化率值显著增加,相较于正常区域有明显的异常增幅。石英脉与其他岩石有较明显的磁性差异,石英脉的磁化率小于0.30×10?3SI,平均为0.10×10?3SI,而其他岩石磁化率一般大于1.0×10?3SI。本研究结合钻孔柱状图与磁化率曲线对比分析,验证了磁化率数据在找矿勘查中的实用价值,为新一轮战略找矿突破提供了科学依据。

    Abstract:

    This study takes the exploration and prospecting work area around the Songjiang River Gold Mine as an example, and through the measurement and comparative analysis of the magnetization rate of three borehole cores, it discusses the application effect of core magnetization rate data in exploration and prospecting.The study used the KT-10 portable magnetization rate instrument from Canada to measure 1,858 core samples, combined with the drilling column diagram and magnetization rate curve comparative analysis. The research results show that: 1) The magnetization rate data has a significant marking effect on the location of pyrite ore, and can effectively indicate the ore-bearing alteration zone; 2) The magnetization rate parameter has an auxiliary role in the division of strata, which helps to distinguish different rock types and structural features. The specific quantitative results are as follows: the maximum value of the magnetic susceptibility data of the ZK1 core is 147.727×10?3 (SI), the minimum value is 0.013×10?3 (SI), and the average value is 2.82482×10?3 (SI). In areas with strong mineralization and alteration (such as 49.00-50.00m, 65.50-67.50m, etc.), the magnetic susceptibility values significantly increase, showing a significant abnormal increase compared to normal areas. Quartz veins have significant magnetic differences from other rocks, with a magnetic susceptibility of less than 0.30×10?3 SI and an average of 0.10×10?3 SI, while the magnetic susceptibility of other rocks is generally greater than 1.0×10?3 SI. This study combines the comparison and analysis of borehole bar charts and magnetic susceptibility curves, verified the practical value of magnetization rate data in exploration and prospection, and provided scientific basis for the new round of strategic exploration breakthrough.

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  • 收稿日期:2025-05-07
  • 最后修改日期:2025-08-13
  • 录用日期:2025-08-14
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