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The magnetotelluric phase tensor

TLDR
In this article, the phase relationship contained in the magnetotelluric (MT) impedance tensor is shown to be a second-rank tensor and the phase tensor can be depicted graphically as an ellipse, the major and minor axes representing the principal axes of the tensor.
Abstract
SUMMARY The phase relationships contained in the magnetotelluric (MT) impedance tensor are shown to be a second-rank tensor. This tensor expresses how the phase relationships change with polarization in the general case where the conductivity structure is 3-D. Where galvanic effects produced by heterogeneities in near-surface conductivity distort the regional MT response the phase tensor preserves the regional phase information. Calculation of the phase tensor requires no assumption about the dimensionality of the underlying conductivity distribution and is applicable where both the heterogeneity and regional structure are 3-D. For 1-D regional conductivity structures, the phase tensor is characterized by a single coordinate invariant phase equal to the 1-D impedance tensor phase. If the regional conductivity structure is 2-D, the phase tensor is symmetric with one of its principal axes aligned parallel to the strike axis of the regional structure. In the 2-D case, the principal values (coordinate invariants) of the phase tensor are the transverse electric and magnetic polarization phases. The orientation of the phase tensor’s principal axes can be determined directly from the impedance tensor components in both 2-D and 3-D situations. In the 3-D case, the phase tensor is nonsymmetric and has a third coordinate invariant that is a distortion-free measure of the asymmetry of the regional MT response. The phase tensor can be depicted graphically as an ellipse, the major and minor axes representing the principal axes of the tensor. 3-D model studies show that the orientations of the phase tensor principal axes reflect lateral variations (gradients) in the underlying regional conductivity structure. Maps of the phase tensor ellipses provide a method of visualizing this variation.

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Citations
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Journal ArticleDOI

Computational recipes for electromagnetic inverse problems

TL;DR: In this paper, a general mathematical framework for Jacobian computations arising in electromagnetic (EM) geophysical inverse problems is developed, which is based on the discrete formulation of the forward problem and divides computations into components (data functionals, forward and adjoint solvers, model parameter mappings).
Journal ArticleDOI

The Magnetotelluric Phase Tensor: A Critical Review

TL;DR: The magnetotelluric phase tensor (MT) is a property of the MT impedance that is resistant to a common form of distortion due to unresolvable local structure.
Journal ArticleDOI

Fluid and deformation regime of an advancing subduction system at Marlborough, New Zealand

TL;DR: The data imply three distinct processes connecting fluid generation along the upper mantle plate interface to rock deformation in the crust as the subduction zone develops, emphasizing the need to include metamorphic and fluid transport processes in geodynamic models.
Journal ArticleDOI

Determinable and non-determinable parameters of galvanic distortion in magnetotellurics

TL;DR: In this article, the phase tensor is used to represent the phase information contained in the impedance of the magnetotelluric (MT) data. But the phase is not the only tensor that can be used for distortion removal.
Journal ArticleDOI

Distribution of melt beneath Mount St Helens and Mount Adams inferred from magnetotelluric data

TL;DR: In this article, the authors used magnetotelluric data recorded at a network of 85 locations in the area of the high conductivity anomaly to infer that the conductivity anomalies associated with the localized zone, and by extension with the mid-crustal conductor, is caused by the presence of partial melt.
References
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Journal ArticleDOI

Decomposition of magnetotelluric impedance tensors in the presence of local three-dimensional galvanic distortion

TL;DR: In this paper, the authors present a decomposition of the magnetotelluric impedance tensor which separates the effects of 3-D channeling from those of 2-D induction.
Journal ArticleDOI

Volcanic and structural evolution of Taupo Volcanic Zone, New Zealand: a review

TL;DR: The history of the Taupo Volcanic Zone (TVZ) can be divided into two categories: the old TVZ from 2.0 Ma to 0.34 Ma and the young TVZ between 0.9 and 0.6 Ma as discussed by the authors.
Journal Article

Interpretation of the magnetotelluric impedance tensor; regional induction and local telluric distortion

TL;DR: In this article, a method for the interpretation of the magnetotelluric (MT) impedance tensor, the telluric-vector technique, is presented, where the phase information of all impedance tensors elements is used to distinguish between local distortion and regional induction, and a model incorporating a superposition of the effects of local surface anomalies and a regional 1D, 2D or 3D conductivity distribution is applied.
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