1887
Volume 20, Issue 1-2
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

A computationally-efficient transformation has been developed to convert coincident loop or in-loop TEM profiles to apparent conductivity versus depth pseudo-sections. The transformation is based on the depth to the maximum physical current induced in a half-space, not on attributes of abstract current filaments. Tests on both synthetic and field data indicate that these pseudo-sections provide a useful qualitative portrayal of conductivity structure, thus facilitating first-pass interpretation of TEM in mapping applications.

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/content/journals/10.1071/EG989043
1989-03-01
2026-01-15
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References

  1. Fullagar, P. K. (1983), ‘Backus-Gilbert inversion of SIROTEM soundings’, A.S.E.G. Third Biennial Conference, Brisbane (abstract).
  2. Macnae, J. and Lamontagne, Y. (1987), ‘Imaging quasi-layered conductive structures by simple processing of TEM data’, Geophysics, 52, 545-554.
  3. Nabighian, M. (1979), ‘Quasi-static transient response of a conducting half-space — an approximate representation’, Geophysics, 44, 1700-1705.
  4. Nekut, A. G. (1987), ‘Direct inversion of time domain electromagnetic data’, Geophysics, 52, 1432-1435.
  5. Raiche, A.P. and Spies, B. R. (1981), ‘Coincident loop transient electromagnetic master curves for interpretation of two-layer earth’, Geophysics, 46, 53-64.
  6. Raiche, A. P. and Gallagher, R. G. (1985), ‘Apparent resistivity and diffusion velocity’, Geophysics 50 1628-1633.
  7. Weidelt, P. (1982), ‘Response characteristics of coincident loop transient electromagnetic systems’, Geophysics, 47, 1325-1330.
/content/journals/10.1071/EG989043
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  • Article Type: Research Article
Keyword(s): apparent conductivity; interpretation; inversion; mapping; pseudo-section; TEM

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