1887
Volume 37, Issue 4
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

We derive an unambiguous apparent conductivity from total magnetic field TEM data for fixed-loop geometry. For single-component fixed-loop TEM measurements, apparent conductivity is either dual-valued or undefined. The ambiguity or non-existence is particularly evident for readings taken outside the transmitter loop, both for step and impulse response data. Therefore, computing apparent conductivity from single-component fixed-loop TEM data can be problematic, especially at intermediate delay times. However, if multi-component fixed-loop magnetic field data is available, an unambiguous apparent conductivity can be derived from | ( )| at all times, except in the inductive limit. Impulse response measurements can be time-weighted and summed to yield “quasi-| |” data. Apparent conductivity derived from quasi-| | amplitudes is dual-valued, but usually only one of the alternatives is geologically plausible. Computing apparent conductivity from | | or quasi-| | amplitudes expedites generation of conductivity-depth sections from fixed-loop TEM. A field data example with multi-component SQUID data shows significant improvement in the conductivity-depth section when | ( )| is transformed rather than the vertical component, B, alone; the lateral extent of a conductive target is under-estimated in the B CDI

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2006-12-01
2026-01-15
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/content/journals/10.1071/EG06348
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  • Article Type: Research Article
Keyword(s): ambiguity; apparent conductivity; fixed loop; TEM; total magnetic field

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