1887
ASEG2012 - 22nd Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Summary

Between 30 and 40% of the Northern Territory is underlain by basalts, mainly the late early Cambrian Kalkarindji Large Igneous Province. These basalts provide a solid floor to mining activities in the overlying strata. They might also provide a buffer of alkalinity and reduction during ore genesis, and should therefore be included in modelling by mineral explorers. A key parameter in the modelling of prospective mineralised zones is the depth to the basalts.

Using the power spectra of open file airborne magnetic data, depths to subsurface basalts can be mapped. A point-and-click package was developed for this purpose, is currently being used to map the depths to the basalts of the Kalkarindji LIP in the Northern Territory.

Open file surveys of magnetic data have varying quality, affecting the ease of extraction of magnetic depths. Although successful depth results can be expected from modern 10 Hz aeromagnetic surveys, the older, 1 Hz proton procession magnetometer data, is more problematic. However some good depth results have been obtained.

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/content/journals/10.1071/ASEG2012ab068
2012-12-01
2026-01-23
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References

  1. Clifton, R., 2007, Depth estimation using the magnetic power spectrum. ASEG Extended Abstracts 2007
  2. Clifton, R., 2010, Modelling ironstone depths using magnetic dipoles. ASEG Extended Abstracts 2010
  3. Kruse, P.D., 1996, Helen Springs stratigraphic drilling 1996 – NTGS96/1 Nilly Waterhole. Northern Territory Geological Survey, Technical Report GS1996-004
  4. Spector, A. and Grant, F.S., 1970, Statistical models for interpreting magnetic data, Geophysics, v. 35, no. 2, pp. 293–302.
/content/journals/10.1071/ASEG2012ab068
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  • Article Type: Research Article
Keyword(s): flood basalts; magnetic depths; power spectra
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