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Volume 22 Number 4
  • E-ISSN: 1365-2478

Abstract

A

Empirical equalities derived from time domain induced polarization scale modelling with the gradient array over simple geometries, and from the potential field functions for equivalent simple charge configurations are similar. The function for the dyke like body is analogous to the magnetic case allowing both total and vertical magnetic field interpretation techniques to be applied to gradient array chargeability anomalies.

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/content/journals/10.1111/j.1365-2478.1974.tb00114.x
2006-04-27
2024-04-19

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References

  1. Bertin, J. and Loeb, J., 1969, Transients and field behaviour in induced polarization, Geophysical Prospecting17, 488–510.
    [Google Scholar]
  2. Grant, F. S. and West, G. F., 1965, Interpretation theory in applied geophysics, McGraw Hill Inc., New York .
    [Google Scholar]
  3. Madden, T. R., Marshall, D. J., Fahlquist, D. A. and Neres, A. S., 1957, Background effects in the induced polarization method of geophysical surveying, A.E.C. rpt. RME—3156.
  4. Moo, J. K. C., 1965, Analytical aeromagnetic interpretation. The inclined prism, Geophysical Prospecting13, 203–224.
    [Google Scholar]
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  • Article Type: Research Article

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