1887

Abstract

Summary

Inverting magnetotelluric (MT) surface data to obtain subsurface resistivity models is a complex and non-linear process where the solution is inherently non-unique. We present a fully data-driven method that enables the direct transformation of MT data into 1D resistivity models using cumulative resistance models. Our approach introduces a cumulative representation of a layered resistivity model, which, at each depth, integrates the effect of overlying layers into the subsurface model. We then establish a relationship between the real part of the TE mode of the MT data and its corresponding cumulative resistance model. Subsequently, we use this relationship to train a neural network that rescales MT data directly into cumulative resistance models. Once the resistance model is retrieved, a numerical derivative is applied to obtain the interval resistivity model, without any prior assumptions about the subsurface structure or resistivity distribution. This approach was validated using both synthetic and real MT datasets, introducing a new perspective for tackling the inversion problem.

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/content/papers/10.3997/2214-4609.202520186
2025-09-07
2026-02-15
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References

  1. Basokur, A.T., Rasmussen, T.M., Kaya, C., Altun, Y. and Aktas, K. [1997] Comparison of induced polarization and controlled-source audio-magnetotellurics methods for massive chalcopyrite exploration in a volcanic area. Geophysics, 62(4), 1087–1096.
    [Google Scholar]
  2. Florio, G. [2018] Mapping the depth to basement by iterative rescaling of gravity or magnetic data. Journal of Geophysical Research: Solid Earth, 123(10), 9101–9120.
    [Google Scholar]
  3. Meju, M.A. [2002] Geoelectromagnetic exploration for natural resources: models, case studies and challenges. Surveys in Geophysics, 23, 133–206.
    [Google Scholar]
  4. Scott, C. [2019] Final Surrender Report E69/2708 for the period 15/09/2011 - 14/09/2019. Statutory annual mineral exploration report, Department of Mines, Industry Regulation and Safety (DMIRS).
    [Google Scholar]
  5. Socco, L. and Comina, C. [2015] Approximate direct estimate of S-wave velocity model from surface wave dispersion curves. In: Near Surface Geoscience 2015-21st European Meeting of Environmental and Engineering Geophysics, 2015. European Association of Geoscientists & Engineers, 1–5.
    [Google Scholar]
  6. Werthmüller, D. [2017] An open-source full 3D electromagnetic modeler for 1D VTI media in Python: empymod. Geophysics, 82(6), WB9–WB19.
    [Google Scholar]
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