1887
ASEG2006 - 18th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

With magnetic gradiometry emerging as a new tool for geophysical exploration, the mathematical modelling of gradient fields is necessary for interpretation of field measurements. Magnetic multipoles may be useful for the modelling of complex geological sources, and so formulae for their field responses are presented here in Cartesian form. The formulae required for the forward modelling of the magnetic gradient tensor can be expressed as a set of linear equations. This fact is exploited to create a hybrid global and local inversion technique whereby simulated multipoles must satisfy the gradient tensor measurements for more than a single measurement.

The inversion process yields subsurface images showing the variation of multipole moment components, as each component is calculated to satisfy measured components of the magnetic gradient tensor. The images exhibit high probability (or small variance) if a multipole is found. The inversion routine is quick, and can be applied automatically to data as it is being collected, or applied to an already complete data set.

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/content/journals/10.1071/ASEG2006ab064
2006-12-01
2026-01-13
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References

  1. Andrew, J. A., Edwards, D. M., Graf, R. J., and Wold, R. J., 1991, Empirical observations relating near-surface magnetic anomalies to high-frequency seismic data and Landsat data in eastern Sheridan County, Montana: Geophysics, 56, ESISTO.
  2. Bellott, A., Corpel, J., and Millon, R., 1991, Contribution of magnetic modelling to the discovery of a hidden massive sulfide body at Hajar, Morocco: Geophysics, 56, 983-991.
  3. Blakely, R., 1996, Potential theory in gravity and magnetic applications: Cambridge University Press.
  4. Carlson, N. R and Zonge, K. L., 2003, Minerals exploration methods modified for environmental targets: Exploration Geophysics, 34, 114-119.
  5. Cowan, E. W., 1968, Basic Electromagnetism: Academic Press Inc.
  6. Doll, W. E., Gamey, T. J., Beard, L. P., and Bell, D. T., 2006, Airborne vertical gradient for near-surface applications: The Leading Edge, 25, 50-53.
  7. Gamey, T. J., Doll, W. E., Beard, L. P., and Bell, D. T., 2002, Airborne vertical magnetic gradient for UXO detection, Proceedings of SAGEEP 2002.
  8. Grauch, V. J. S. and Millegan, P. S., 1998, Mapping intrabasinal faults from high-resolution aeromagnetic data: The Leading Edge, 17, 53-55.
  9. Gunn, P., 1998, Aeromagnetics locates prospective areas and prospects: The Leading Edge, 17, 67-69.
  10. Halliday, D., Resnick, R., and Walker, J., 1997, Fundamentals of Physics: John Wiley & Sons, Inc.
  11. Heath, P. J., Heinson, G., and Greenhalgh, S. A., 2003, Some comments on potential field tensor data: Exploration Geophysics, 34, 57-62.
  12. Schmidt, P., Clark, D., Leslie, K., Bick, M., Tilbrook, D., and Foley, C, 2004, GETMAG a SQUID magnetic tensor gradiometer for mineral and oil exploration: Exploration Geophysics, 35, 297-305.
  13. Schmidt, P. W. and Clark, D. A., 2000, Advantages of measuring the magnetic gradient tensor: Preview, 85, 26-30.
  14. Schmidt, P. W. and Clark, D. A., 2006, The magnetic gradient tensor: Its properties and uses in source characterization: The Leading Edge, 25, 75-78.
  15. Telford, W. M., Geldart, L. P., and Sherrif, R. E., 1996, Applied Geophysics: Cambridge University Press.
  16. Tsokas, G. N., Stampolidis, A., Angelopoulos, A. D., and Kilias, S., 1998, Analysis of potential field anomalies in Lavrion mining area, Greece: Geophysics, 63, 1965-1970.
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  • Article Type: Research Article
Keyword(s): Forward modelling; Inversion; Multipoles
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