强剩磁条件的非凸优化反演方法研究
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    摘要:

    剩余磁化强度是常见岩石物理属性,构建强剩磁场源模型对于深部地质结构和矿产资源探测具有重要意义。磁异常模量稀疏反演是获取高分辨率剩磁模型的有效方法,其本质是磁性模型的L0范数极小。但L0范数计算求解困难,传统方法通过凸近似函数逼近L0范数,虽能实现目标函数梯度的稳定计算,却难以控制反演模型体积。本文构建了包含数据拟合项、模型约束项和L0范数约束项的磁异常模量反演优化模型,采用迭代硬阈值方法实现L0范数的稳定迭代计算,从而实现强剩磁条件反演模型边界的清晰刻画及尺度可控。研究表明,该方法可在保证数据拟合精度的前提下,实现模型尺度渐近线性收敛,从而获得目标体积的强剩磁反演模型。通过理论模型实验验证了方法有效性与稳定性;并应用于江苏冶山地区,构建了成矿岩体的磁性模型,为深部找矿提供了科学依据。

    Abstract:

    Remanent magnetization is a common rock physical property, and constructing a strong remanent magnetic field source model is crucial for deep geological structure and mineral resource exploration. Sparse inversion of magnetic anomaly modulus is an effective method for generating remanent magnetization models with high resolution, which essentially minimizes the L0 norm of the model. However, the computation of the L0 norm is challenging, and traditional methods approximate it using convex functions. While this allows for stable gradient calculation of the objective function, it is difficult to control the volume of the inverted model. This paper proposes a magnetic anomaly modulus inversion optimization model that includes data fitting, model constraints, and L0 norm constraints. The method utilizes an iterative hard thresholding approach to achieve stable iterative calculation of the L0 norm, enabling clear delineation of the inversion model boundary under strong remanent magnetization conditions while controlling its scale. The study shows that this method ensures accurate data fitting and achieves asymptotic linear convergence of model scale, leading to a strong remanent magnetization inversion model of the target volume. The method’s effectiveness and stability were validated through theoretical model experiments. It was then applied to the Yeshan area in Jiangsu, where a magnetic model of the mineralization body was constructed, providing scientific evidence for deep mineral exploration.

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  • 收稿日期:2025-07-11
  • 最后修改日期:2025-10-12
  • 录用日期:2025-10-14
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