1887
Volume 12, Issue 4
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

Abstract

Two functions, H(x) and V(x) involving the combinations of both the horizontal T(x) and vertical T(x) gradients of the total magnetic intensity anomaly due to a buried sloping step are defined as

H(x) = T(x) cos 2/β + T(x) sin 2/β and

V(x) = T (x) cos 2/β - T (x) sin 2/β

where β is the effective inclination of the magnetization vector. By combining the two gradients T(x) and T(x) in this fashion the effect of inclination of the inducing field is removed in the two functions H(x) and V(x). Characteristic points on H(x) and V(x) curves such as zero crossings and equi-gradients are used to evaluate the parameters of the step. This technique can be extended easily to magnetic anomalies in vertical and horizontal components.

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/content/journals/10.1071/EG981089
1981-12-01
2026-01-16
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References

  1. Grant, F. S. & West, G. F. (1965), Interpretation Theory in Applied Geophysics, McGraw Hill Co., New York.
  2. Green, R. (1980), ‘Field processing of magnetic data’, Geophys. Prosp. 28,384-91.
  3. Green, R. & Stanley, J. M. (1975), ‘Application of a Hilbert transform method to the interpretation of surface-vehicle magnetic data’, Geophys. Prosp. 23, 18-27.
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  5. Hall, D. H. (19686), ‘Regional magnetic anomalies, magnetic units and crustal structure in the Kenora district of Ontario’, Can. J. Earth Sci. 5, 1277-96.
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  7. Hood, P. (1965), ‘Gradient measurements in aeromagnetic surveying’. Geophysics 30, 891-902.
  8. Hood, P. & McClure, D. J. (1965), ‘Gradient measurements in ground magnetic prospecting’. Geophysics 30, 403-10.
  9. Murthy, I. V. R. & Rao, C. V. (1974), ‘A note on the (sin x)/x method of continuation’, Boll. Di Geofisica Teorica Ed Applicata 16,223-31.
/content/journals/10.1071/EG981089
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  • Article Type: Research Article

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