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Volume 8 Number 4
  • E-ISSN: 1365-2478

Abstract

A

Let be a system of rectangular axes with origin at the earth's surface and with the axis pointing vertically downwards. If a body lies wholly] between the planes =, = then for all x, y and for = 1, 2, 3 it is proved that

where =/, β=/ and is the gravitational constant. D are very easily computed from the Bouger anomaly and J are tabulated in this paper.

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2006-04-27
2024-04-28

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References

  1. Bott, M. H. P., and SmithR.A., 1958. The estimation of the limiting depth of gravitating bodies. Geophysical Prospecting, 6, 1–10.
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  2. Bullard, E. C. and Cooper, R. I. B., 1948. The determination of the masses necessary to produce a given gravitational field. Proc. Roy. Soc. A., 194, 341.
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  3. Coulomb, J., 1958. Sur la profondeur ?un corps produissant une anomalie gravimetrique. Comptes Rendus Acad. Sci. Paris, 247 (No. 8), 719–720 and 247 (No. 17), 1370.
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  4. Smith, R. A., 1959. Some depth formulae for local magnetic and gravity anomalies. Geophysical Prospecting, 7, 55–63.
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  • Article Type: Research Article

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