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    金属矿山深部断层三维结构重建的深度卡尔曼滤波法:以胶东半岛夏甸金矿为例

    刘启亮 陈玉铉 刘占坤 毛先成 邓敏

    刘启亮, 陈玉铉, 刘占坤, 毛先成, 邓敏, 2026. 金属矿山深部断层三维结构重建的深度卡尔曼滤波法:以胶东半岛夏甸金矿为例. 地球科学, 51(3): 940-954. doi: 10.3799/dqkx.2026.028
    引用本文: 刘启亮, 陈玉铉, 刘占坤, 毛先成, 邓敏, 2026. 金属矿山深部断层三维结构重建的深度卡尔曼滤波法:以胶东半岛夏甸金矿为例. 地球科学, 51(3): 940-954. doi: 10.3799/dqkx.2026.028
    Liu Qiliang, Chen Yuxuan, Liu Zhankun, Mao Xiancheng, Deng Min, 2026. Deep Learning Aided Kalman Filter for 3D Detailed Modelling of Deep Fault in Metal Mines: A Case Study from the Xiadian Gold Deposit, Jiaodong Peninsula, Eastern China. Earth Science, 51(3): 940-954. doi: 10.3799/dqkx.2026.028
    Citation: Liu Qiliang, Chen Yuxuan, Liu Zhankun, Mao Xiancheng, Deng Min, 2026. Deep Learning Aided Kalman Filter for 3D Detailed Modelling of Deep Fault in Metal Mines: A Case Study from the Xiadian Gold Deposit, Jiaodong Peninsula, Eastern China. Earth Science, 51(3): 940-954. doi: 10.3799/dqkx.2026.028

    金属矿山深部断层三维结构重建的深度卡尔曼滤波法:以胶东半岛夏甸金矿为例

    doi: 10.3799/dqkx.2026.028
    基金项目: 

    湖南省自然科学基金重点项目 2026JJ30010

    深地国家科技重大专项课题 2025ZD1008208

    详细信息
      作者简介:

      刘启亮(1986-),男,教授,博士,从事地学数据挖掘与统计相关研究工作. ORCID:0000-0002-4684-8504. E-mail:qiliang.liu@csu.edu.cn

      通讯作者:

      刘占坤,ORCID:0000-0002-3734-1138. E-mail:zkliu0322@csu.edu.cn

    • 中图分类号: P612

    Deep Learning Aided Kalman Filter for 3D Detailed Modelling of Deep Fault in Metal Mines: A Case Study from the Xiadian Gold Deposit, Jiaodong Peninsula, Eastern China

    • 摘要:

      为了解决金属矿山深部直接观测缺乏、间接观测不确定性高,深部构造难以精细化三维重建的问题,利用先验知识弥补数据缺陷,研发了深度卡尔曼滤波法.基于卡尔曼滤波的思想,将由浅部到深部的断层三维建模视为“时序预测”问题:(1)结合浅部断层和产状约束,构建预测深部断层位置的状态方程;(2)借助物探推断数据和卷积网络代替观测,构建观测方程.通过融合预测和观测结果,实现深部断层位置的最优推断.该模型在夏甸金矿的应用表明:建模结果在深部钻孔揭露的断裂位置平均水平误差为6.17 m,精度较隐式建模方法提升91%~93%,能更准确反映深部断层的精细形态特征.基于重建的模型,在夏甸矿区深部圈定出四个成矿潜力区,可为后续资源勘查提供指导.

       

    • 图  1  深度卡尔曼滤波法总体框架

      Fig.  1.  Workflow for DLAKF

      图  2  产状约束示意

      a.产状约束剖面;b.产状约束平面

      Fig.  2.  Schematic diagram of occurrence constraint

      图  3  融合骨架线约束的空间注意力卷积网络结构

      Fig.  3.  The structure of spatial attention convolutional network with skeleton constraint

      图  4  夏甸金矿床地质平面图及剖面图

      图改自Liu et al.(2021);a.夏甸金矿床地质平面图;b.夏甸金矿床剖面图

      Fig.  4.  Geological plan and profile of Xiadian gold deposit

      图  5  骨架线和验证钻孔

      a.不含验证钻孔的骨架线;b.含验证钻孔的骨架线

      Fig.  5.  Skeletons and verification drill holes

      图  6  损失函数曲线

      a.训练集损失函数曲线;b.测试集损失函数曲线

      Fig.  6.  Loss curves

      图  7  ‒1 200 m至‒3 000 m深部断层模型水平投影图

      a.倾角等值线图;b.走向等值线图

      Fig.  7.  Plan views of deep fault model from ‒1 200 m to ‒3 000 m

      图  8  深部断层产状统计直方图

      a.倾角分布直方图;b.走向分布直方图

      Fig.  8.  Histogram of deep fault occurrence

      图  9  深部断层水平误差

      a.1号钻孔水平误差;b.2号钻孔水平误差;c.3号钻孔水平误差

      Fig.  9.  Horizontal error of deep fault

      图  10  深度卡尔曼滤波法及对比方法重建三维模型

      a.深度卡尔曼滤波(‒1 200~‒3 000 m);b.径向基插值(‒1 000~‒2 500 m);c.克里金插值(‒1 000~‒2 500 m);d.离散光滑插值(‒1 000~‒2 500 m)

      Fig.  10.  3D models generated by the DLAKF and comparison methods

      图  11  深度卡尔曼滤波法重建断层与视电阻率剖面对比

      a.勘探线A解算的视电阻率剖面;b.勘探线B解算的视电阻率剖面

      Fig.  11.  Comparison of the DLAKF model and apparent resistivity profile

      图  12  断层整体三维模型(200 m至‒3 000 m)及矿化关联散点图

      a.断层三维模型及金矿化分布;b. dF与矿化关联散点图;c. gF与矿化关联散点图;d. cF与矿化关联散点图;e. wF与矿化关联散点图

      Fig.  12.  3D model of fault (200 m to ‒3 000 m) and mineralization correlation scatter plot

      图  13  深部成矿潜力靶区水平投影图(黄色区域)

      Fig.  13.  Plan view of favourable metallogenic zones (yellow zones) inferred based on the DLAKF model

      表  1  深部断层水平误差

      Table  1.   Horizontal error table of deep faults

      钻孔编号 钻孔深度(m) 深度卡尔曼滤波(m) 骨架线模型(m) 径向基插值(m) 克里金插值(m) 离散光滑插值(m)
      1 ‒1 288.82 9.64 35.90 65.62 57.38 64.01
      2 ‒1 333.35 4.51 38.33 9.99 31.40 29.04
      3 ‒2 251.40 4.37 31.32 195.39 119.54 173.33
      平均 6.17 35.18 90.33 69.44 88.79
      下载: 导出CSV
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