1887
Volume 19, Issue 1-2
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

Conventional downhole EM surveys measure only one component of the EM field aligned with the drill hole axis. Consequently interpretations are often inconclusive. Three-component downhole TEM surveys can overcome the rotational ambiguities associated with current filament inversions. However, suitable probes are difficult to construct. New sensors have now been developed incorporating sensitive preamplifiers. Orthogonal components can be measured sequentially and the orientation of the probe can be determined using an absolute gravity reference. The system has been tested in a ground traverse over a major conductor and the results are consistent with the response obtained using coincident loop techniques.

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/content/journals/10.1071/EG988051
1988-03-01
2026-01-22
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References

  1. Barnett, C. T. (1984)—‘Simple inversion of time-domain electromagnetic data’, Geophysics 49, 925–933.
  2. Cull, J. P. & Cobcroft, Ft. (1986)—‘Omni-directional downhole EM probes’, Geophysical Prospecting 34, 569–579.
  3. Duncan, A. C. (1986)—‘Filament inversion of fixed-loop TEM data’, unpublished Monash University honours thesis.
  4. Hoschke, T. (1985)—‘A new drill hole magnetometer: preliminary results from the Tennant Creek area’, Exploration Geophysics 16, 365–374.
  5. McCracken, K. G., Hohmann, G. W. & Oristaglio, M. L. (1980)—‘Why time domain?’, Exploration Geophysics 11, 318–321.
/content/journals/10.1071/EG988051
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  • Article Type: Research Article

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