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Chapter 10: Analysis of MT Data

Published:
January 01, 2002

10.1 QUESTIONS AND STAGES IN MAGNETOTELLURIC INTERPRETATION

The impedance tensor, [Z], and the Wiese-Parkinson matrix (the tipper), [W], are determined as functions of the period, T. Interpretation of these functions leads to the construction of a geoelectric model for the region under study. This procedure consists of three basic steps.

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Investigations in Geophysics

Magnetotellurics in the Context of the Theory of Ill-Posed Problems

Mark N. Berdichevsky
Mark N. Berdichevsky
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;
Vladimir I. Dmitriev
Vladimir I. Dmitriev
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Society of Exploration Geophysicists
Volume
11
ISBN electronic:
9781560802068
Publication date:
January 01, 2002

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