A reduced order approach for probabilistic inversions of 3-D magnetotelluric data I: general formulation

Author:

Manassero M C1ORCID,Afonso J C12,Zyserman F3ORCID,Zlotnik S4,Fomin I1

Affiliation:

1. Australian Research Council Centre of Excellence for Core to Crust Fluid Systems/GEMOC, Department of Earth and Environmental Sciences, Macquarie University, 2109, Sydney, Australia

2. Centre for Earth Evolution and Dynamics, Department of Geosciences, University of Oslo, 0315, Oslo, Norway

3. CONICET, Facultad de Ciencias Astronómicas y Geofísicas, Universidad de La Plata, 1900, La Plata, Argentina

4. Laboratori de Càlcul Numèric, Escola Tècnica Superior d’Enginyers de Camins, Canals i Ports, Universitat Politècnica de Catalunya, 08034, Barcelona, Spain

Abstract

SUMMARY Simulation-based probabilistic inversions of 3-D magnetotelluric (MT) data are arguably the best option to deal with the nonlinearity and non-uniqueness of the MT problem. However, the computational cost associated with the modelling of 3-D MT data has so far precluded the community from adopting and/or pursuing full probabilistic inversions of large MT data sets. In this contribution, we present a novel and general inversion framework, driven by Markov Chain Monte Carlo (MCMC) algorithms, which combines (i) an efficient parallel-in-parallel structure to solve the 3-D forward problem, (ii) a reduced order technique to create fast and accurate surrogate models of the forward problem and (iii) adaptive strategies for both the MCMC algorithm and the surrogate model. In particular, and contrary to traditional implementations, the adaptation of the surrogate is integrated into the MCMC inversion. This circumvents the need of costly offline stages to build the surrogate and further increases the overall efficiency of the method. We demonstrate the feasibility and performance of our approach to invert for large-scale conductivity structures with two numerical examples using different parametrizations and dimensionalities. In both cases, we report staggering gains in computational efficiency compared to traditional MCMC implementations. Our method finally removes the main bottleneck of probabilistic inversions of 3-D MT data and opens up new opportunities for both stand-alone MT inversions and multi-observable joint inversions for the physical state of the Earth’s interior.

Funder

ARC

European Space Agency

CONICET

Horizon 2020

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

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