1887

Abstract

Summary

A concept of the frequency-normalized impedance (FNI) function is introduced for the visualization of all components of the magnetotelluric impedance tensor. This definition provides some useful properties to obtain an initial information for the subsurface resistivity distribution.

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/content/papers/10.3997/2214-4609.201414159
2015-10-05
2024-04-18
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References

  1. Basokur, A. T.
    [1994] Definitions of apparent resistivity for the presentation of magnetotelluric sounding data. Geophysical Prospecting, 42, 141–149.
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  2. [1999] Properties of the magnetotelluric frequency-normalised impedance function over a layered medium. Journal of the Balkan Geophysical Society, 2, 63–74. (available at http://www.balkangeophysoc.gr/)
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  3. Cagniard, L.
    [1953] Basic theory of the magnetotelluric method of geophysical prospecting. Geophysics, 18, 605–635.
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