The Determination and Application of Vector Gravity Anomalies

Conventional gravity measurements are only of the maximum magnitude of the gravity acceleration vector. This is because the gravimeter is aligned with the gravity vector and not in a self consistent reference frame. However, when a high-resolution geoid model is available, vector gravity data can be...

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Main Authors: Featherstone, Will, Dentith, M., Kirby, Jon
Format: Journal Article
Published: CSIRO Publishing 2000
Subjects:
Online Access:http://www.publish.csiro.au/nid/225/issue/4489.htm
http://hdl.handle.net/20.500.11937/39862
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author Featherstone, Will
Dentith, M.
Kirby, Jon
author_facet Featherstone, Will
Dentith, M.
Kirby, Jon
author_sort Featherstone, Will
building Curtin Institutional Repository
collection Online Access
description Conventional gravity measurements are only of the maximum magnitude of the gravity acceleration vector. This is because the gravimeter is aligned with the gravity vector and not in a self consistent reference frame. However, when a high-resolution geoid model is available, vector gravity data can be computed. The geoid model is used to compute the deflections of the gravity vector from the ellipsoidal normal, thus providing direction to the measured magnitude of gravity acceleration. This allows the components of the gravity vector to be computed from the gravity measurements. Since the geoid is mostly generated by deeper Earth structure, the components of the vector gravity anomaly enhance the information on deeper mass variations above that contained in the conventional gravity anomaly. This approach has been applied to the Australian gravity database and shows a number of linear features not clearly evident in conventional Bouguer gravity anomaly maps.
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publishDate 2000
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spelling curtin-20.500.11937-398622017-01-30T14:37:49Z The Determination and Application of Vector Gravity Anomalies Featherstone, Will Dentith, M. Kirby, Jon regional interpretation Geoid vector gravity anomalies Conventional gravity measurements are only of the maximum magnitude of the gravity acceleration vector. This is because the gravimeter is aligned with the gravity vector and not in a self consistent reference frame. However, when a high-resolution geoid model is available, vector gravity data can be computed. The geoid model is used to compute the deflections of the gravity vector from the ellipsoidal normal, thus providing direction to the measured magnitude of gravity acceleration. This allows the components of the gravity vector to be computed from the gravity measurements. Since the geoid is mostly generated by deeper Earth structure, the components of the vector gravity anomaly enhance the information on deeper mass variations above that contained in the conventional gravity anomaly. This approach has been applied to the Australian gravity database and shows a number of linear features not clearly evident in conventional Bouguer gravity anomaly maps. 2000 Journal Article http://hdl.handle.net/20.500.11937/39862 http://www.publish.csiro.au/nid/225/issue/4489.htm CSIRO Publishing restricted
spellingShingle regional interpretation
Geoid
vector gravity anomalies
Featherstone, Will
Dentith, M.
Kirby, Jon
The Determination and Application of Vector Gravity Anomalies
title The Determination and Application of Vector Gravity Anomalies
title_full The Determination and Application of Vector Gravity Anomalies
title_fullStr The Determination and Application of Vector Gravity Anomalies
title_full_unstemmed The Determination and Application of Vector Gravity Anomalies
title_short The Determination and Application of Vector Gravity Anomalies
title_sort determination and application of vector gravity anomalies
topic regional interpretation
Geoid
vector gravity anomalies
url http://www.publish.csiro.au/nid/225/issue/4489.htm
http://hdl.handle.net/20.500.11937/39862