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可控源音频大地电磁法和微动谱比法的横向约束联合反演

王崇龙 彭淼

世界核地质科学2025,Vol.42Issue(3):565-581,17.
世界核地质科学2025,Vol.42Issue(3):565-581,17.DOI:10.3969/j.issn.1672-0636.2025.03.008

可控源音频大地电磁法和微动谱比法的横向约束联合反演

Laterally constrained joint inversion of CSAMT and microtremor spectrum method

王崇龙 1彭淼2

作者信息

  • 1. 中国地质大学(北京)地球物理与信息技术学院,北京 100083||核工业二四○研究所,辽宁 沈阳 110000
  • 2. 中国地质大学(北京)地球物理与信息技术学院,北京 100083
  • 折叠

摘要

Abstract

In order to make the distribution of lateral physical properties and layer parameters between adjacent measuring points smoother and more continuous and reduce the limitations of a single geophysical inversion method,a pseudo-two-dimensional lateral constrained joint inversion study of controlled source audio frequency magnetotelluric method(CSAMT)and micro-motion spectrum ratio method was carried out.The microtremor data is numerically simulated using the spectral ratio method,combined with the CSAMT-based limited memory BFGS(L-BFGS)inversion algorithm,introducing the lateral constraint theory,and adding the cross-gradient function to achieve the mutual coupling of two different physical parameters.A set of quasi-two-dimensional lateral constraint joint inversion algorithms was developed,and the accuracy and effectiveness of the algorithms were verified through two sets of theoretical models.Meanwhile,the inversion algorithm is used to invert the measured data in Yanqing,Beijing.The results show that there is a good correspondence between the abrupt interface morphology of resistivity and shear wave velocity,which proves the practical value of the laterally constrained joint inversion algorithm.

关键词

可控源音频大地电磁法/微动/横向约束/联合反演

Key words

controlled source audio magnetotelluric method/microtremor/laterally constraint/joint inversion

分类

天文与地球科学

引用本文复制引用

王崇龙,彭淼..可控源音频大地电磁法和微动谱比法的横向约束联合反演[J].世界核地质科学,2025,42(3):565-581,17.

基金项目

国家自然科学基金项目(编号:42174086)资助 Supported by National Natural Science Foundation of China(No.42174086) (编号:42174086)

世界核地质科学

1672-0636

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