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

Abstract

Finite difference and integral equation methods are used to model electromagnetic wave propagation in a disrupted coal seam. The results show that easily detectable changes of electromagnetic signals will occur if a modest geological anomaly (e.g. a 60 × 6 × 2 m3 dyke) disrupts the seam.

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/content/journals/10.1071/EG991247
1991-03-01
2026-01-21
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References

  1. Greenfield, R. J., and Wu, S. T., (1988). ‘Electromagnetic wave propagation in disrupted coal seams’. Extended Abstracts of the 57th Internat. Annual Meeting, New Orleans.
  2. Newman, G. A., Hohmann, G. W., and Anderson, W. L., (1986). Transient electromagnetic response of a three-dimensional body in a layered earth’. Geophysics51, 1608-1627.
  3. Smith, G. H., Williamson, P. R., and Vozoff, K., (1990). The application of nested dissection to the solution of a 2V2-D electromagnetic problem’. Submitted to Applied Computational Electromagnetics.
  4. Stolarczyk, L. G., Rogers G., and Hatherly, P., (1988). ‘Comparison of radio imaging method (RIM) electromagnetic wave tomography with in-mine geological mapping in the Liddell, Bulli and Wongawilli coal seams’. Explor. Geophys., 19, 169-170.
  5. Stoyer, C. H., and Greenfield, R. J., (1976). ‘Numerical solutions of the response of a two-dimensional earth to an oscillating magnetic dipole source’. Geophysics41, 519-530.
/content/journals/10.1071/EG991247
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  • Article Type: Research Article
Keyword(s): coal; disruption; electromagnetic; wave

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