ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    基于机器学习和黄铁矿微量元素识别金矿床类型

    Classification of Gold Deposit Types Based on Machine Learning and Pyrite Trace Element Geochemistry

    • 摘要: 黄铁矿是金矿床中最常见的载金矿物,其地球化学成分能有效指示成矿信息。笔者系统收集了全球浅成低温热液型、斑岩型和造山型金矿床中黄铁矿的微量元素数据,选取9种常见的地球化学特征,采用K近邻算法、随机森林和支持向量机3种机器学习模型进行模型训练,旨在建立一种基于黄铁矿成分高效、准确识别金矿床类型的新方法。模型分类性能评估结果显示,训练得到的K近邻算法、随机森林和支持向量机模型的分类准确率分别为0.89、0.96和0.95。此外,文中采用未参与训练的东昆仑造山型金矿黄铁矿成分对训练模型进行独立验证,以评估其在实际应用中的适用性与准确性。结果表明,3种模型均能正确识别出这些黄铁矿主要来源于造山型金矿,其中支持向量机模型效果最佳,准确率达0.88。为克服机器学习的“黑匣子”问题,文中还引入机器学习可解释性方法,以揭示不同黄铁矿微量元素输入特征对分类结果的贡献度。SHAP分析表明,在识别斑岩型和造山型金矿时,对模型输出结果影响最大的3个黄铁矿微量元素特征依次为As、Co和Cu,而在识别浅成低温热液型金矿时,黄铁矿的Cu、As和Ni含量对模型输出结果影响最大。研究结果表明,黄铁矿微量元素可作为区分金矿成因类型的有效标志。未来,结合机器学习方法,黄铁矿成分有望进一步拓展至其他类型矿床的识别与分类,为矿床成因研究与找矿预测提供新的技术途径。

       

      Abstract: Pyrite is the most common gold bearing mineral in gold deposits, and its geochemical composition can effectively indicate mineralization processes. This study systematically compiles trace element data of pyrite from epithermal, porphyry, and orogenic gold deposits worldwide. Nine commonly used geochemical features are selected, and three machine learning models including the K nearest neighbors algorithm, random forest, and support vector machine are employed for model training, with the aim of establishing an efficient and accurate method for identifying gold deposit types based on pyrite composition. The evaluation results of model classification performance show that the classification accuracies of the trained K nearest neighbors, random forest, and support vector machine models are 0.89, 0.96, and 0.95, respectively. In addition, pyrite compositional data from the East Kunlun orogenic gold deposits that are not involved in model training are used for independent validation to assess the applicability and accuracy of the models in practical scenarios. The results indicate that all three models correctly identify these pyrites as mainly derived from orogenic gold deposits, among which the support vector machine model achieves the best performance with an accuracy of 0.88. To address the black box issue in machine learning, an interpretable machine learning method is further introduced to quantify the contributions of different pyrite trace element features to the classification results. The SHAP analysis reveals that As, Co, and Cu are the three most influential trace element features for distinguishing porphyry and orogenic gold deposits, whereas Cu, As, and Ni exert the greatest influence on the identification of epithermal gold deposits. The results demonstrate that trace elements in pyrite can serve as effective indicators for discriminating genetic types of gold deposits. In the future, combined with machine learning approaches, pyrite composition has the potential to be further extended to the identification and classification of other types of mineral deposits, providing new technical approaches for studies on ore genesis and mineral exploration prediction.

       

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