Analysis of Different Methodologies to Calculate Bouguer Gravity Anomalies in the Argentine Continental Margin

Autores
Pedraza De Marchi, Ana Carolina; Ghidella, Marta E.; Tocho, Claudia Noemí
Año de publicación
2014
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
We have tested and used two methods to determine the Bouguer gravity anomaly in the area of the Argentine continental margin. The first method employs the relationship between the topography and gravity anomaly in the Fourier transform domain using Parker’s expression for different orders of expansion. The second method computes the complete Bouguer correction (Bullard A, B and C) with the Fortran code FA2BOUG2. The Bouguer slab correction (Bullard A), the curvature correction (Bullard B) and the terrain correction (Bullard C) are computed in several zones according to thedistances between the topography and the calculation point. In each zone, different approximations of the gravitationalattraction of rectangular or conic prisms are used according to the surrounding topography. Our calculations show that the anomaly generated by the fourth order in Parker’s expansion is actually compatible with the traditional Bouguer anomaly calculated with FA2BOUG, and that higher orders do not introduce significant changes. The comparison reveals that the difference between both methods in the Argentine continental margin has a quasi bimodal statistical distribution. The main disadvantage in using routines based on Parker's expansion is that an average value of the topography is needed for the calculation and, as the margin has an abrupt change of the topography in the continental slope area, it causes a bimodal distribution. It is worth noticing that, as expected, the most important differences between both methods are located over the continental slope both in complex structures such as part of the shared margin, as well as in isolated points where there are contributions from short wavelength or rugged topography.
Facultad de Ciencias Astronómicas y Geofísicas
Materia
Geofísica
Bouguer anomaly
Argentine continental margin
Parker’s expansion
Grdfft3
Gravfft1
FA2BOUG
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by-nc-sa/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/101655

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oai_identifier_str oai:sedici.unlp.edu.ar:10915/101655
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network_name_str SEDICI (UNLP)
spelling Analysis of Different Methodologies to Calculate Bouguer Gravity Anomalies in the Argentine Continental MarginPedraza De Marchi, Ana CarolinaGhidella, Marta E.Tocho, Claudia NoemíGeofísicaBouguer anomalyArgentine continental marginParker’s expansionGrdfft3Gravfft1FA2BOUGWe have tested and used two methods to determine the Bouguer gravity anomaly in the area of the Argentine continental margin. The first method employs the relationship between the topography and gravity anomaly in the Fourier transform domain using Parker’s expression for different orders of expansion. The second method computes the complete Bouguer correction (Bullard A, B and C) with the Fortran code FA2BOUG2. The Bouguer slab correction (Bullard A), the curvature correction (Bullard B) and the terrain correction (Bullard C) are computed in several zones according to thedistances between the topography and the calculation point. In each zone, different approximations of the gravitationalattraction of rectangular or conic prisms are used according to the surrounding topography. Our calculations show that the anomaly generated by the fourth order in Parker’s expansion is actually compatible with the traditional Bouguer anomaly calculated with FA2BOUG, and that higher orders do not introduce significant changes. The comparison reveals that the difference between both methods in the Argentine continental margin has a quasi bimodal statistical distribution. The main disadvantage in using routines based on Parker's expansion is that an average value of the topography is needed for the calculation and, as the margin has an abrupt change of the topography in the continental slope area, it causes a bimodal distribution. It is worth noticing that, as expected, the most important differences between both methods are located over the continental slope both in complex structures such as part of the shared margin, as well as in isolated points where there are contributions from short wavelength or rugged topography.Facultad de Ciencias Astronómicas y Geofísicas2014-04info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf33-41http://sedici.unlp.edu.ar/handle/10915/101655enginfo:eu-repo/semantics/altIdentifier/url/https://ri.conicet.gov.ar/11336/32781info:eu-repo/semantics/altIdentifier/issn/2163-1697info:eu-repo/semantics/altIdentifier/doi/10.5923/j.geo.20140402.02info:eu-repo/semantics/altIdentifier/hdl/11336/32781info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-29T11:20:01Zoai:sedici.unlp.edu.ar:10915/101655Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-29 11:20:02.012SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv Analysis of Different Methodologies to Calculate Bouguer Gravity Anomalies in the Argentine Continental Margin
title Analysis of Different Methodologies to Calculate Bouguer Gravity Anomalies in the Argentine Continental Margin
spellingShingle Analysis of Different Methodologies to Calculate Bouguer Gravity Anomalies in the Argentine Continental Margin
Pedraza De Marchi, Ana Carolina
Geofísica
Bouguer anomaly
Argentine continental margin
Parker’s expansion
Grdfft3
Gravfft1
FA2BOUG
title_short Analysis of Different Methodologies to Calculate Bouguer Gravity Anomalies in the Argentine Continental Margin
title_full Analysis of Different Methodologies to Calculate Bouguer Gravity Anomalies in the Argentine Continental Margin
title_fullStr Analysis of Different Methodologies to Calculate Bouguer Gravity Anomalies in the Argentine Continental Margin
title_full_unstemmed Analysis of Different Methodologies to Calculate Bouguer Gravity Anomalies in the Argentine Continental Margin
title_sort Analysis of Different Methodologies to Calculate Bouguer Gravity Anomalies in the Argentine Continental Margin
dc.creator.none.fl_str_mv Pedraza De Marchi, Ana Carolina
Ghidella, Marta E.
Tocho, Claudia Noemí
author Pedraza De Marchi, Ana Carolina
author_facet Pedraza De Marchi, Ana Carolina
Ghidella, Marta E.
Tocho, Claudia Noemí
author_role author
author2 Ghidella, Marta E.
Tocho, Claudia Noemí
author2_role author
author
dc.subject.none.fl_str_mv Geofísica
Bouguer anomaly
Argentine continental margin
Parker’s expansion
Grdfft3
Gravfft1
FA2BOUG
topic Geofísica
Bouguer anomaly
Argentine continental margin
Parker’s expansion
Grdfft3
Gravfft1
FA2BOUG
dc.description.none.fl_txt_mv We have tested and used two methods to determine the Bouguer gravity anomaly in the area of the Argentine continental margin. The first method employs the relationship between the topography and gravity anomaly in the Fourier transform domain using Parker’s expression for different orders of expansion. The second method computes the complete Bouguer correction (Bullard A, B and C) with the Fortran code FA2BOUG2. The Bouguer slab correction (Bullard A), the curvature correction (Bullard B) and the terrain correction (Bullard C) are computed in several zones according to thedistances between the topography and the calculation point. In each zone, different approximations of the gravitationalattraction of rectangular or conic prisms are used according to the surrounding topography. Our calculations show that the anomaly generated by the fourth order in Parker’s expansion is actually compatible with the traditional Bouguer anomaly calculated with FA2BOUG, and that higher orders do not introduce significant changes. The comparison reveals that the difference between both methods in the Argentine continental margin has a quasi bimodal statistical distribution. The main disadvantage in using routines based on Parker's expansion is that an average value of the topography is needed for the calculation and, as the margin has an abrupt change of the topography in the continental slope area, it causes a bimodal distribution. It is worth noticing that, as expected, the most important differences between both methods are located over the continental slope both in complex structures such as part of the shared margin, as well as in isolated points where there are contributions from short wavelength or rugged topography.
Facultad de Ciencias Astronómicas y Geofísicas
description We have tested and used two methods to determine the Bouguer gravity anomaly in the area of the Argentine continental margin. The first method employs the relationship between the topography and gravity anomaly in the Fourier transform domain using Parker’s expression for different orders of expansion. The second method computes the complete Bouguer correction (Bullard A, B and C) with the Fortran code FA2BOUG2. The Bouguer slab correction (Bullard A), the curvature correction (Bullard B) and the terrain correction (Bullard C) are computed in several zones according to thedistances between the topography and the calculation point. In each zone, different approximations of the gravitationalattraction of rectangular or conic prisms are used according to the surrounding topography. Our calculations show that the anomaly generated by the fourth order in Parker’s expansion is actually compatible with the traditional Bouguer anomaly calculated with FA2BOUG, and that higher orders do not introduce significant changes. The comparison reveals that the difference between both methods in the Argentine continental margin has a quasi bimodal statistical distribution. The main disadvantage in using routines based on Parker's expansion is that an average value of the topography is needed for the calculation and, as the margin has an abrupt change of the topography in the continental slope area, it causes a bimodal distribution. It is worth noticing that, as expected, the most important differences between both methods are located over the continental slope both in complex structures such as part of the shared margin, as well as in isolated points where there are contributions from short wavelength or rugged topography.
publishDate 2014
dc.date.none.fl_str_mv 2014-04
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info:eu-repo/semantics/publishedVersion
Articulo
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://sedici.unlp.edu.ar/handle/10915/101655
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dc.language.none.fl_str_mv eng
language eng
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info:eu-repo/semantics/altIdentifier/issn/2163-1697
info:eu-repo/semantics/altIdentifier/doi/10.5923/j.geo.20140402.02
info:eu-repo/semantics/altIdentifier/hdl/11336/32781
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by-nc-sa/4.0/
Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by-nc-sa/4.0/
Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
dc.format.none.fl_str_mv application/pdf
33-41
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