1887
2nd Australasian Exploration Geoscience Conference: Data to Discovery
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Summary

Following advances in magnetometer instrumentation and inversion software we re-explore the feasibility of a field methodology utilising relationships between magnetization and dynamic (time-variation) magnetic field anomalies to recover structural information from magnetic field data over thin sheets. We show that we can estimate the dip of a sheet from a reliably determined dynamic magnetic anomaly induced by the range of the magnetic field through its diurnal variation. The strength and inclination of remanent magnetization in the plane perpendicular to the sheet can be subsequently estimated from the static magnetic anomaly using that pre-determined dip angle. The principal challenge in working with dynamic magnetic anomalies is their low amplitude and the requirement for multiple measurements at each station. These relationships between magnetizations and fields apply equally to field gradients. SQUID magnetometers and gradiometers can provide a feasible solution to the high resolution measurements required for this application

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/content/journals/10.1080/22020586.2019.12073127
2019-12-01
2026-01-23
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References

  1. Billings et al, 2012. Superconducting Magnetic Tensor Gradiometer System for Detection of Underwater Military Munitions, SERDP Project MR-1661.
  2. Clark, D. A., Schmidt, P. W., Coward, D. A. and Huddleston, M. P., 1998. Remote determination of magnetic properties and improved drill targeting of magnetic anomaly sources by Differential Vector Magnetometry (DVM). Exploration Geophysics, 29, 312-319.
  3. Clark, D.A., 2014. Methods for determining remanent and total magnetisations of magnetic sources - a review. Exploration Geophysics, 45, 271–304. http://dx.doi.org/10.1071/EG14013.
  4. Emerson, D. W., Clark, D. A., and Saul, S. J., 1985, Magnetic exploration models incorporating remanence, demagnetisation and anisotropy: HP 41C handheld computer algorithms: Exploration Geophysics, 16, 1–122. doi:10.1071/EG985001
  5. Goldstein, N.E. and Ward, S.H., 1966. The separation of remanent from induced magnetization in situ. Geophysics, 31, 779-796.
  6. Hall, D.H., 1959, Direction of polarization determined from magnetic anomalies: Journal of Geophysical Research, 64, 1945-1959. doi:10.1029/JZ064i011p01945
  7. Keenan, S.T., Du, J., Mitchell, E.E.,, Lam, K.H., Macfarlane, J.C., Lewis, C.J., Leslie, K.E., and Foley, C.P., 2013. High-Tc Superconducting Electronic Devices Based on YBCO Step-Edge Grain Boundary Junctions IEICE Trans. Electron., VOL.E96–C, NO.3.
  8. Keenan, S., Leslie, K., and Clark, D., 2015. Single sensor HTS SQUID magnetic tensor gradiometer. In: European Conference on Applied Superconductivity (EUCAS); 6-10 September; Lyon, France. IEEE Transactions on Applied Superconductivity; 2015. 1. https://publications.csiro.au/rpr/download?pid=csiro:EP152283&dsid=DS5
  9. Leslie, K., Blay, K.; Clark, D., Schmidt, P., Tilbrook, D., and Foley, C. P., 2007. Helicopter trial of magnetic tensor gradiometer. 19th International Geophysical Conference & Exhibition (ASEG 2007); Perth, WA.
  10. McGrath, P. H., & Hood, P. J. (1970). The dipping dike case: a computer curve-matching method of magnetic interpretation. Geophysics, 35(5), 831-848.
  11. Muhling, P.C., Brakel, A.T., and Davidson, A.W., 1978, Mount Egerton, Western Australia Sheet SG50-3, 1:250,000 explanatory series, Geological Survey of Western Australia.
  12. Parkinson, W.D. and Barnes, C.D., 1985. In situ determination of Koenigsberger ratio. Australian Journal of Earth Science, 32, 1-5.
  13. Tilbrook, D.L., 2004. The design of a new concept HTSC axial gradiometer. Physica C, 407, 1-9.
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  • Article Type: Research Article
Keyword(s): SQUID magnetic anomaly sheet remanent magnetization time-variation
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