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Related Concept Videos

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Two-dimensional Bayesian inversion of magnetotelluric data using trans-dimensional Gaussian processes.

Daniel Blatter1, Anandaroop Ray2, Kerry Key1

  • 1Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY, 10964, USA.

Geophysical Journal International
|May 17, 2021
PubMed
Summary
This summary is machine-generated.

We developed a new 2-D Bayesian inversion for magnetotelluric data, using Gaussian processes for efficient subsurface resistivity modeling. This method provides crucial uncertainty information for 2-D earth models.

Keywords:
Electrical propertiesInverse theoryMagnetotelluricsNon-linear electromagneticsProbability distributions

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Area of Science:

  • Geophysics
  • Electromagnetism
  • Computational Science

Background:

  • Bayesian inversion of electromagnetic data is vital for subsurface resistivity uncertainty.
  • High computational costs limit Bayesian methods to 1-D models.
  • 2-D and 3-D inversions remain computationally challenging.

Purpose of the Study:

  • To demonstrate the first fully 2-D, trans-dimensional Bayesian inversion of magnetotelluric (MT) data.
  • To make computationally expensive Bayesian inversions tractable for 2-D resistivity models.
  • To quantify subsurface electrical resistivity uncertainty in 2-D.

Main Methods:

  • Utilized a Gaussian process (GP) for parsimonious model parametrization.
  • Employed a trans-dimensional, parallel tempered Markov chain Monte Carlo sampler.
  • Integrated GP with the MARE2DEM finite element forward solver for dense mesh computations.

Main Results:

  • Successfully inverted synthetic and field MT data for 2-D electrical resistivity models.
  • Achieved a parameter reduction of over 32× compared to traditional methods.
  • Generated resistivity probability distributions quantifying 2-D model uncertainty.

Conclusions:

  • The novel trans-dimensional GP sampler enables computationally tractable 2-D Bayesian MT inversion.
  • The method provides quantitative uncertainty information crucial for geophysical interpretation.
  • This technique can inform estimations of subsurface physical properties like porosity and fluid content.