1887
  1. Home
  2. A-Z Publications
  3. Geophysical Prospecting
  4. Volume 29, Issue 3
  5. Article
Volume 29 Number 3
  • E-ISSN: 1365-2478

Abstract

A

The gravity anomaly caused by a deviation of a density interface that is of constant profile but finite extension (a so‐called 2 1/2‐dimensional structure) can be expressed in polynomial form that can be inverted. Numerical experiments with synthetic structures show the viability of this inversion method.

Loading

Article metrics loading...

/content/journals/10.1111/j.1365-2478.1981.tb01022.x
2006-04-27
2024-04-27

  • From This Site

    /content/journals/10.1111/j.1365-2478.1981.tb01022.x
    dcterms_title,dcterms_subject,pub_keyword
    -contentType:Journal -contentType:Contributor -contentType:Concept -contentType:Institution
    10
    5
Loading full text...

Full text loading...

References

  1. Rarnold, J.1975, On estimation of the degree of best polynomials, XVI General Assembly of IUGG, IAG.
  2. Baldi, P. and Unguendoli, M.1978, Inversion of gravity profiles by polynomial method, Geophysical Prospecting26, 247–251.
    [Google Scholar]
  3. Bullard, E.C. and Cooper, R.I.B.1948, The determination of the masses necessary to produce a given gravitational field, Proceedings of the Royal Society194, 332–347.
    [Google Scholar]
  4. Nagy, D.1966, The gravitational attraction of a right rectangular prism, Geophysics31, 362–371.
    [Google Scholar]
  5. Pick, M., Picha, J. and Vyskocil, V.1973, Theory of the Earth's Gravity Field, Elsevier.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/journals/10.1111/j.1365-2478.1981.tb01022.x
Loading
  • Article Type: Research Article

Most Cited This Month Most Cited RSS feed

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error