1887
ASEG2003 - 16th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Negative responses recorded during moving in-loop TEM surveys, where only positive data are expected, are a regular occurrence in TEM surveys. They are however generally poorly understood and little reported. In most cases, such negatives are ascribed to induced polarisation (IP) effects, but we suggest that there is at least one other cause of negative TEM response, one which is associated with very resistive terranes containing little if any polarisable material.

This paper presents some examples of this negative resistive response where there is little or no polarisable material present and where a source other than IP should be sought. A series of tests have been proposed to try and isolate the cause.

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/content/journals/10.1071/ASEG2003ab014
2003-08-01
2026-01-16
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References

  1. Bishop, J.R., Enright, M.J., Hinks, J.D. and Kakebeeke, V.Q., 2001. A report on the 2001 SEM, DHEM and DHMMR surveys at Kakoulima, Guinea. RTME report.
  2. Bishop, J.R., Hinks, J.D. and Mclntosh, S.M., 2002. Kakoulima: A Resistive Regime for EM. RTME report.
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  5. Jansen, J.C. and Doyle, B.J., 1998. The Tli Kwi Cho kimberlite complex, Northwest Territories, Canada: a geophysical post mortum. In: Northwest Mining Association 1998 Practical Geophysics Short Course, edited by R.B. Ellis, R. Irvine and F. Fritz.
  6. Kakebeeke, V.Q. and Mclntosh, S.M., 2000. Kakoulima, Guinea TEM survey. RTME report.
  7. Smith, R. S., and West, G. F., 1989, Field examples of negative coincident-loop transient electromagnetic anomalies modelled with polarisable half-planes: Geophysics, 54, 1491-1498.
  8. Weidelt, P., 1982, Response characteristics of coincident-loop transient EM systems: Geophysics, 47, 1325-1330.
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  • Article Type: Research Article
Keyword(s): kimberlites; negative responses; nickel; resistive terranes; ultramafics
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