Spectral methods in gravity inversion: the geopotential field and its derivatives

The 3D spectral analysis of the gravitational potential field for a given mass distribution is studied. The derived quantities, the gravitational force field and the gravity gradient tensor are computed in frequency space. As an example, the fields are theoretically and numerically evaluated for a r...

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Main Authors: C. Braitenberg, M. Zadro
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1997-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3875
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author C. Braitenberg
M. Zadro
author_facet C. Braitenberg
M. Zadro
author_sort C. Braitenberg
collection DOAJ
description The 3D spectral analysis of the gravitational potential field for a given mass distribution is studied. The derived quantities, the gravitational force field and the gravity gradient tensor are computed in frequency space. As an example, the fields are theoretically and numerically evaluated for a right rectangular prism. The spectral approach finds several geophysical applications, as, e.g., in inversion processes. Gravity inversion for deep seated masses, as for instance at Moho level, are treated with an iterative inversion process, in which the downward continuation is alternated with the classical calculation of the gravity field. The theory is applied to the inversion of the gravity data in the SE-Alps, regarding only the long-period field, generated by Moho undulations. The results are used for the evaluation of the equipotential lines, the gravity field, and the gravity gradient tensor in a vertical section of the Alpine crustal root.
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spelling doaj.art-b2085488b5d84990951e3578b31961f12022-12-21T17:58:23ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X1997-06-0140510.4401/ag-3875Spectral methods in gravity inversion: the geopotential field and its derivativesC. BraitenbergM. ZadroThe 3D spectral analysis of the gravitational potential field for a given mass distribution is studied. The derived quantities, the gravitational force field and the gravity gradient tensor are computed in frequency space. As an example, the fields are theoretically and numerically evaluated for a right rectangular prism. The spectral approach finds several geophysical applications, as, e.g., in inversion processes. Gravity inversion for deep seated masses, as for instance at Moho level, are treated with an iterative inversion process, in which the downward continuation is alternated with the classical calculation of the gravity field. The theory is applied to the inversion of the gravity data in the SE-Alps, regarding only the long-period field, generated by Moho undulations. The results are used for the evaluation of the equipotential lines, the gravity field, and the gravity gradient tensor in a vertical section of the Alpine crustal root.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3875gravity inversiondownward continuationgravitational gradient tensor
spellingShingle C. Braitenberg
M. Zadro
Spectral methods in gravity inversion: the geopotential field and its derivatives
Annals of Geophysics
gravity inversion
downward continuation
gravitational gradient tensor
title Spectral methods in gravity inversion: the geopotential field and its derivatives
title_full Spectral methods in gravity inversion: the geopotential field and its derivatives
title_fullStr Spectral methods in gravity inversion: the geopotential field and its derivatives
title_full_unstemmed Spectral methods in gravity inversion: the geopotential field and its derivatives
title_short Spectral methods in gravity inversion: the geopotential field and its derivatives
title_sort spectral methods in gravity inversion the geopotential field and its derivatives
topic gravity inversion
downward continuation
gravitational gradient tensor
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3875
work_keys_str_mv AT cbraitenberg spectralmethodsingravityinversionthegeopotentialfieldanditsderivatives
AT mzadro spectralmethodsingravityinversionthegeopotentialfieldanditsderivatives