高级检索

基于贝叶斯优化随机森林算法的多源数据岩性识别研究以集宁浅覆盖区为例

Research on lithology identification using multi-source data based on Bayesian-optimized random forest algorithm—A case study of Jining shallow overburden area

  • 摘要: 内蒙古集宁地区是华北克拉通北缘重要的钼多金属矿产地之一,具有较大钼多金属矿成矿潜力。然而,该区地表覆盖的新生代玄武岩和碎屑沉积物对成矿信息具有屏蔽和衰减作用。在传统岩性识别方法中,仅依靠单一类型数据,难以满足覆盖区资源勘查的复杂应用需求。因此,须联合遥感和重磁异常数据,对集宁浅覆盖区基于贝叶斯优化的随机森林算法展开岩性识别研究。针对集宁浅覆盖区的遥感和重磁异常数据进行处理及多源数据融合,设置试验区并开展多源数据智能岩性识别方法有效性分析。通过精度评价,对比不同特征组合的分类精度,并分析不同特征在岩性分类中的重要性。将基于贝叶斯优化随机森林算法用于整个集宁浅覆盖区多源数据融合的岩性分类。结果表明,与使用单一类型数据相比,该方法得出的岩性识别结果更优,F1值达到0.885,同时优化了集宁浅覆盖区花岗岩分布情况,使得岩性边界更加清晰。研究成果对地质勘查工作具有应用价值与指导意义。

     

    Abstract: The Jining area of Inner Mongolia is one of the significant molybdenum polymetallic mining regions along the northern margin of the North China Craton, exhibiting considerable potential for molybdenum polymetallic mineralization. However, the Cenozoic basalts and clastic sediments covering the surface in this area obscure and attenuate mineralization-related information. Traditional lithology identification methods relying solely on a single type of data struggle to meet the complex demands of resource exploration in overburden regions. Therefore, this study integrated remote sensing and gravity-magnetic anomaly data to conduct lithology identification research using a random forest algorithm optimized iteratively via Bayesian optimization for the Jining shallow overburden area. Remote sensing and gravity-magnetic anomaly data from the study area were processed and fused with other multi-source data. Then, a test area was established to analyze the effectiveness of the intelligent lithology identification method based on multi-source data. Through accuracy evaluation, the classification performance of different feature combinations was compared and analyzed, and the importance of various features in lithology classification was assessed. Finally, the Bayesian-optimized random forest algorithm was applied to lithology classification using fused multi-source data across the entire study area. The results indicate that compared to using only a single type of data, this method yields the optimal lithology identification outcome, with F1 value reaching 0.885. It also refines the distribution of granite in the study area, resulting in clearer lithological boundaries. This research provides valuable insights and guidance for geological exploration in the region.

     

/

返回文章
返回