1887
Volume 22, Issue 1
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

Regional aeromagnetic interpretation includes an important mapping component as well as location of possible economic targets. Given these varied requirements, objective interpretation techniques based on spectral analysis and application of specialised filters play a major role. Recent improvements in computer hardware, particularly microcomputers, have made it possible to analyse more data and it is now feasible to perform quantitative analysis on complete blocks of aeromagnetic data. Quantitative analysis may be applied to profile or grid data or both, depending on the interpretation objectives and the data quality. Results are presented for two analytical interpretation techniques, location of the maxima of the pseudo-gravity gradient and 3D Euler deconvolution. These results together with apparent susceptibility mapping provide objective information on geological boundaries, depths and lithologies.

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/content/journals/10.1071/EG991081
1991-03-01
2026-01-15
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References

  1. Blakely, R. J., and Simpson, R. W., (1986). ‘Approximating edges of source bodies from magnetic or gravity anomalies.’ Geophysics51, 1494-1498.
  2. Cowan, D. R., Kane, M. G., Merghelani, H., and Pitkin, J. A., (1985). ‘Regional aeromagnetic/radiometric surveys: a perspective.’ First Break.3, 17-21.
  3. Reid, A. B., Allsop, J. M, Granser, H., Millett, A. J., and Somerton, I. W, (1990). ‘Magnetic interpretation in three dimensions using Euler deconvolution.’ Geophysics55, 80-91.
  4. Thompson, D. T, (1982). ‘EULDPH – A new technique for making computer assisted depth estimates from magnetic data.’ Geophysics47, 31-37.
/content/journals/10.1071/EG991081
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  • Article Type: Research Article
Keyword(s): aeromagnetics; Brazil; Euler deconvolution; gradient maxima; Middle East; shield area; Yilgarn

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