1887
Volume 30 Number 6
  • E-ISSN: 1365-2478

Abstract

A

Magnetotelluric response is studied for an inhomogeneous medium having conductivity varying linearly with depth as σ() =σ. For a medium having conductivity increasing linearly with depth, the phase of the impedance approaches 60° at long periods and the apparent resistivity becomes log (ρ) = 2 log (1.36/α1/3) — 1/3 log ('). The asymptote of log (ρ, '→∞) when plotted against log (') has a constant gradient —1/3 and has an intercept on the log (') axis, which equals 6 log (1.36/α1/3). When a homogeneous layer with a moderate thickness overlies an inhomogeneous half‐space, this layer does not affect the asymptote, but it affects the cut‐off period and pushes this toward the long period direction. For a medium having conductivity decreasing linearly with depth, the impedance is equivalent to that of a Cagniard two‐layer model; the intercept period related to the thickness is '(/2)2. Homogeneous multilayer approximations to an inhomogeneous layer are also investigated, and it is shown that the fit to the model variation depends on the number of layers and the layer parameters chosen.

Loading

Article metrics loading...

/content/journals/10.1111/j.1365-2478.1982.tb01344.x
2006-04-27
2024-04-23
Loading full text...

Full text loading...

References

  1. Abramovici, F.1974, The forward magnetotelluric problem for an inhomogeneous and anisotropic structure, Geophysics39, 56–68.
    [Google Scholar]
  2. Berdichevskiy, M. I., Dmitriyev, V. I. and Mershchikova, N. A.1974, Investigation of gradient media in deep electromagnetic sounding, Izvestiya Akademii Nauk SSSR, Fizika Zemli6, 61–72. (English Translation: Bulletin of the Academy of Sciences of the USSR, Physics of Solid Earth, 6, 380–386, 1974.).
    [Google Scholar]
  3. Bossy, L. and De Vuyst, A.1959. Relations entre les champs élèctrique et magnetique d'une onde de periode très lonque induits dans un milieu de conductivité variable, Pure and Applied Geophysics44, 119–134.
    [Google Scholar]
  4. Cagniard, L.1953, Basic theory of the magnetotelluric method of geophysical prospecting, Geophysics18, 605–635.
    [Google Scholar]
  5. Fischer, G. and Le Quang, B. V.1981, Topography and minimization of a standard deviation in one‐dimensional magnetotelluric modelling, Geophysical Journal of the Royal Astronomical Society67, 279–292.
    [Google Scholar]
  6. Kao, D.1981, Magnetotelluric response on vertically inhomogeneous earth, Journal of Geophysical Research86, B4, 3027–3038.
    [Google Scholar]
  7. Kao, D. and Rankin, D.1980, Magnetotelluric response on inhomogeneous layered earth, Geophysics45, 1793–1802.
    [Google Scholar]
  8. Mallick, K.1970, Magnetotelluric sounding on a layered earth with transitional boundary, Geophysical Prospecting18, 738–757.
    [Google Scholar]
  9. Patra, H. P. and Mallick, K.1980, Geosounding Principles 2, Time‐Varying Geoelectric Soundings, Elsevier, Amsterdam , Oxford , New York .
    [Google Scholar]
http://instance.metastore.ingenta.com/content/journals/10.1111/j.1365-2478.1982.tb01344.x
Loading
  • Article Type: Research Article

Most Cited This Month Most Cited RSS feed

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error