Quasi-two-dimensional joint inversion of the data from the controlled source audio-frequency magnetotellurics and the microtremor survey

ZHANG Ji-Wei; TAN Hui

doi:10.11720/wtyht.2024.1477

2024 Vol. 48, No. 4

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Article navigation > Geophysical and Geochemical Exploration > 2024 > 48(4): 1094-1102

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ZHANG Ji-Wei, TAN Hui. 2024. Quasi-two-dimensional joint inversion of the data from the controlled source audio-frequency magnetotellurics and the microtremor survey. Geophysical and Geochemical Exploration, 48(4): 1094-1102. doi: 10.11720/wtyht.2024.1477

Citation:

ZHANG Ji-Wei, TAN Hui. 2024. Quasi-two-dimensional joint inversion of the data from the controlled source audio-frequency magnetotellurics and the microtremor survey. Geophysical and Geochemical Exploration, 48(4): 1094-1102. doi: 10.11720/wtyht.2024.1477

Quasi-two-dimensional joint inversion of the data from the controlled source audio-frequency magnetotellurics and the microtremor survey

Institute of Urban Underground Space and Energy Studies, The Chinese University of Hong Kong (Shenzhen ), Shenzhen 518172, China

Received Date: 10 November 2023

Revised Date: 29 December 2023

Abstract

Abstract

Both the controlled source audio-frequency magnetotellurics (CSAMT) and the microtremor survey exhibit promising application prospectsunder strong urban interference. However, single geophysical inversion methods are challenged by a multiplicity of solutions. To achieve the complementary advantages of different geophysical methods, and address the lateral discontinuity of single-point inversion, this studyexplored the quasi-two-dimensional joint inversion of the CSAMTand microtremor survey data. It enabled the joint inversionby introducing a lateral constraint matrix into the objective function for joint inversion and employing the limited-memory Broyden-Fletcher-Goldfarb-Shanno (LBFGS) algorithm. The reliability and effectiveness of the joint inversion were verified using the inversion example of synthetic data from theoretical models. The results show that compared to single data inversion, the joint inversion can effectively improve the accuracy of inversion results, with the resistivity model more consistent with theshear-wave velocity structure. Moreover, lateral constraints can effectively reduce the discontinuity of the physical parameters of adjacentsurvey points. The quasi-two-dimensional joint inversion with lateral constraints enhances the inversion reliability by obtaining more reasonable profile results of physical parameters and structures with the efficiency of single-point inversion.
- joint inversion /
- controlled source audio-frequency magnetotellurics /
- microtremor survey /
- laterally constrained inversion

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References

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