1887
Volume 38, Issue 4
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

Three-dimensional (3D) high-susceptibility tabular models of Banded Iron Formation (BIF) were built for the area of an aeromagnetic survey at the Musselwhite Mine, Ontario. The study used all available drill information to create geologically plausible models built from a central axis of nodes with geometrical and susceptibility attributes assigned to each node. The forward total magnetic intensity was then computed using an algorithm that includes a calculation for the demagnetisation effect. The model-building process greatly enhanced the understanding of the BIF geometry and demonstrated the importance of the interaction of these strongly magnetic units with the Earth’s magnetic field. As BIF is associated with mineralisation at the mine, the interpretation of the observed magnetic anomalies has strong implications for target generation.

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/content/journals/10.1071/EG07027
2007-12-01
2026-01-17
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References

  1. Clark D. A. Emerson D. W. 1991 Notes on Rock Magnetism Characteristics in Applied Geophysical Studies: Exploration Geophysics 22 547 555
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  2. Logan K. J. , and Angus R. 1997, An iterative method to calculate self-demagnetisation for 3D magnetic bodies, with application to the Osborne copper gold deposit: 12th Australian Society Exploration Geophysics Conference Preview 66, p. 95.
  3. Telford W. M. , Geldart L. P. , and Sheriff R. E. 1990, Applied Geophysics Cambridge University Press, Second edition, p 104–106.
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  • Article Type: Research Article
Keyword(s): Banded Iron Formation; demagnetisation; magnetics; modelling; Musselwhite

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