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
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/101655
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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 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Articulo http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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http://sedici.unlp.edu.ar/handle/10915/101655 |
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http://sedici.unlp.edu.ar/handle/10915/101655 |
dc.language.none.fl_str_mv |
eng |
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eng |
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