反演(地质)
皮尔逊积矩相关系数
正规化(语言学)
图像分辨率
反变换采样
计算机科学
算法
遥感
地球物理学
地质学
数学
人工智能
统计
地震学
电信
构造学
表面波
作者
Yunhe Liu,Xu Na,Changchun Yin,Yang Su,Siyuan Sun,Bo Zhang,Xiuyan Ren,Vikas Chand Baranwal
标识
DOI:10.1109/tgrs.2022.3143659
摘要
Based on the spatial structure correlation in different geophysical parameters, we propose a new 3-D joint inversion method for frequency-domain airborne electromagnetic (AEM) and airborne magnetic (AirMag) data by incorporating a local Pearson correlation constraint (LPCC). For each iteration, the entire model is separated into multiple subdomains and the Pearson correlation coefficients of resistivity and magnetization in the subdomain are employed as the additional regularization term to do the joint constraint. This new regularization term is continuously updated in the inversion process to ensure that the resistivity and magnetization models in two separated inversions converge to a similar spatial structure. As a statistics technology, the LPCC-based joint inversion scheme not only has the advantages of the conventional joint inversions, but also can implement the structural constraints in different scales by selecting different sizes of the subdomain. This provides the flexibility for solving multiscale problems. Synthetic examples show that the joint inversion can improve the overall inversion resolution by combining the high vertical resolution of the EM method and large exploration depth and high horizontal resolution of the magnetic method. In the application to field survey datasets, the joint inversion delivers better results than those of separate inversions, which further verifies the effectiveness of our method.
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