1887
ASEG2001 - 15th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Based on the newly defined formula of a spherical Bouguer anomaly, the authors have proposed a new method intending to determine the regional VGG anomaly and the Bouguer density so as to satisfy the condition of eliminating the topographic gravitational effects. For this purpose, we have introduced a new concept of ‘the datum level such that the value of the Bouguer anomaly becomes invariant for any Bouguer density’, and have shown an approximate equation to be satisfied by and Also, we have shown an explicit formula to estimate These two simultaneous equations enable us to estimate both and These quantities and subsequently conducted gravity corrections will give a new way to construct Bouguer anomaly distribution with no gravitational effect due to topographic undulation.

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/content/journals/10.1071/ASEG2001ab095
2001-12-01
2026-01-17
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References

  1. Nozaki, K., 1981, A computer program for spherical terrain correction, Jour, of the Geodetic Society of Japan, 27, 23-32.
  2. Nozaki, K., 1999, A note on the basic characteristics of spherical gravity corrections: gravitational behavior of a thin spherical cap of axial symmetry, Jour, of the Geodetic Society of Japan, 45, 215-266.
  3. Nozaki, K., 2001, Generalized Bouguer gravity anomaly (1): formulation of spherical Bouguer anomaly reduced onto an arbitrary equi-potential surface, ASEG 15 Geophysical Conference and Exhibition, Brisbane, Extended Abstracts.
  4. Tsuboi, C. 1965, Calculation of Bouguer anomalies with due regard to the anomaly in the vertical gravity gradient, Japan Academic Proceedings, 41, 386-391.
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