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A stable finite element solution for two-dimensional magnetotelluric modelling

Abstract
Summary. We report herein on a finite element algorithm for 2-D magnetotelluric modelling which solves directly for secondary variations in the field parallel to strike, plus the subsequent vertical and transverse auxiliary fields, for both transverse electric and transverse magnetic modes. The governing Helmholtz equations for the secondary fields along strike are the same as those for total field algorithms with the addition of source terms involving the primary fields and the conductivity difference between the body and the host. Our approach has overcome a difficulty with numerical accuracy at low frequencies observed in total field solutions with 32-bit arithmetic far the transverse magnetic mode especially, but also for the transverse electric mode. Matrix ill-conditioning, which affects total field solutions, increases with the number of element rows with the square of the maximum element aspect ratio and with the inverse of frequency. In the secondary formulation, the field along strike and the auxiliary fields do not need to be extracted in the face of an approximately computed primary field which increasingly dominates the total field solution towards low frequencies. In addition to low-frequency stability, the absolute accuracy of our algorithm is verified by comparison with the TM and the TE mode analytic responses of a segmented overburden model.

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Citations
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Journal ArticleDOI

Occam's inversion to generate smooth, two-dimensional models from magnetotelluric data

TL;DR: In this paper, the authors propose an extension of the existing 1-D algorithm, Occam's inversion, to smooth 2-D models using an extension to the existing Occam inversion.
Journal ArticleDOI

Fluid generation and pathways beneath an active compressional orogen, the New Zealand Southern Alps, inferred from magnetotelluric data

TL;DR: In this article, two independent, two-dimensional inversion algorithms were applied to the wideband magnetotelluric (MT) data, and both imply a concave-upward (U-shaped), middle to lower crustal conductive zone beneath the west central portion of the island.
Journal ArticleDOI

Marine magnetotellurics for petroleum exploration Part I: A sea-floor equipment system

TL;DR: In this paper, the authors used ac-coupled sensors, induction coils for the magnetic field, and an electric field amplifier developed for marine controlled-source applications for seafloor magnetotelluric measurements.
Journal ArticleDOI

Resistivity cross section through the Juan de Fuca Subduction System and its tectonic implications

TL;DR: In this paper, a resistivity cross section to depths exceeding 200 km has been derived from magnetotelluric observations along a profile near latitude 45oN from the Juan de Fuca spreading center, across the coastal subduction complex, the High Cascades volcanic arc, and into the back-arc Deschutes Basin region.
Journal ArticleDOI

A parallel goal-oriented adaptive finite element method for 2.5-D electromagnetic modelling

TL;DR: A parallel goal-oriented adaptive finite element method that can be used to rapidly compute highly accurate solutions for 2.5-D controlled-source electromagnetic (CSEM) and 2-D magnetotelluric modelling problems.
References
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Book

The finite element method for engineers

TL;DR: The Finite Element Method as discussed by the authors is a method to meet the Finite Elements Method of Linear Elasticity Theory (LETI) and is used in many of the problems of mesh generation.
Dissertation

A magnetotelluric investigation of an electrical conductivity anomaly in the southwestern United States

TL;DR: Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Geology and Geophysics, 1967 as discussed by the authors, Boston, Massachusetts, U.S.
Journal ArticleDOI

Electromagnetic and electrical modeling by the finite element method

J. H. Coggon
- 01 Feb 1971 - 
TL;DR: In this article, it is shown that a solution for secondary rather than total field quantities can be obtained directly by using the finite element method to solve the electromagnetic energy minimization problem.
Journal ArticleDOI

Magnetotelluric responses of three-dimensional bodies in layered earths

TL;DR: The electromagnetic fields scattered by a three-dimensional inhomogeneity in the earth are affected strongly by boundary charges as discussed by the authors, which causes tensor magnetotelluric (MT) apparent resistivities to remain anomalous as frequency approaches zero.
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