Numerical modeling for the upper crustal deformation in the Southern Andes
- Autores
- Quinteros, J.; Ramos, V.A.; Jacovkis, P.M.
- Año de publicación
- 2005
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- In this work, the modeling of plate tectonic processes associated with crustal deformation through a numerical framework for non-collisional Andean type orogens is presented. The main objectives of the numerical framework are to develop a numerical model in order to represent large-scale deformation in Andean type subduction zones, to include appropriate physical and mathematical laws that describe the behavior of the lithosphere, to model surface erosion taking into account dominant winds direction and the synorogenic topography of the orogen as the crustal erosion caused by friction between the subducting and the overriding plate and to include isostatic compensation behavior taking into account flexural rigidity. © 2005 Asociación Geológica Argentina.
Fil:Quinteros, J. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Ramos, V.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Jacovkis, P.M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. - Fuente
- Rev. Asoc. Geol. Argent. 2005;60(4):714-723
- Materia
-
Deformation
Erosion
Finite elements
Isostasy
Viscoplastic rheology
Andean orogeny
crustal deformation
deformation
erosion
finite element method
flexure
isostasy
lithosphere
numerical model
plate tectonics
rheology
subduction zone
viscoplasticity
Andes
South America - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by/2.5/ar
- Repositorio
- Institución
- Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
- OAI Identificador
- paperaa:paper_00044822_v60_n4_p714_Quinteros
Ver los metadatos del registro completo
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Numerical modeling for the upper crustal deformation in the Southern Andes Quinteros, J.Ramos, V.A.Jacovkis, P.M.DeformationErosionFinite elementsIsostasyViscoplastic rheologyAndean orogenycrustal deformationdeformationerosionfinite element methodflexureisostasylithospherenumerical modelplate tectonicsrheologysubduction zoneviscoplasticityAndesSouth AmericaIn this work, the modeling of plate tectonic processes associated with crustal deformation through a numerical framework for non-collisional Andean type orogens is presented. The main objectives of the numerical framework are to develop a numerical model in order to represent large-scale deformation in Andean type subduction zones, to include appropriate physical and mathematical laws that describe the behavior of the lithosphere, to model surface erosion taking into account dominant winds direction and the synorogenic topography of the orogen as the crustal erosion caused by friction between the subducting and the overriding plate and to include isostatic compensation behavior taking into account flexural rigidity. © 2005 Asociación Geológica Argentina.Fil:Quinteros, J. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.Fil:Ramos, V.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.Fil:Jacovkis, P.M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.2005info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfhttp://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p714_QuinterosRev. Asoc. Geol. Argent. 2005;60(4):714-723reponame:Biblioteca Digital (UBA-FCEN)instname:Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturalesinstacron:UBA-FCENenginfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/2.5/ar2025-09-29T13:42:52Zpaperaa:paper_00044822_v60_n4_p714_QuinterosInstitucionalhttps://digital.bl.fcen.uba.ar/Universidad públicaNo correspondehttps://digital.bl.fcen.uba.ar/cgi-bin/oaiserver.cgiana@bl.fcen.uba.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:18962025-09-29 13:42:53.345Biblioteca Digital (UBA-FCEN) - Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturalesfalse |
dc.title.none.fl_str_mv |
Numerical modeling for the upper crustal deformation in the Southern Andes |
title |
Numerical modeling for the upper crustal deformation in the Southern Andes |
spellingShingle |
Numerical modeling for the upper crustal deformation in the Southern Andes Quinteros, J. Deformation Erosion Finite elements Isostasy Viscoplastic rheology Andean orogeny crustal deformation deformation erosion finite element method flexure isostasy lithosphere numerical model plate tectonics rheology subduction zone viscoplasticity Andes South America |
title_short |
Numerical modeling for the upper crustal deformation in the Southern Andes |
title_full |
Numerical modeling for the upper crustal deformation in the Southern Andes |
title_fullStr |
Numerical modeling for the upper crustal deformation in the Southern Andes |
title_full_unstemmed |
Numerical modeling for the upper crustal deformation in the Southern Andes |
title_sort |
Numerical modeling for the upper crustal deformation in the Southern Andes |
dc.creator.none.fl_str_mv |
Quinteros, J. Ramos, V.A. Jacovkis, P.M. |
author |
Quinteros, J. |
author_facet |
Quinteros, J. Ramos, V.A. Jacovkis, P.M. |
author_role |
author |
author2 |
Ramos, V.A. Jacovkis, P.M. |
author2_role |
author author |
dc.subject.none.fl_str_mv |
Deformation Erosion Finite elements Isostasy Viscoplastic rheology Andean orogeny crustal deformation deformation erosion finite element method flexure isostasy lithosphere numerical model plate tectonics rheology subduction zone viscoplasticity Andes South America |
topic |
Deformation Erosion Finite elements Isostasy Viscoplastic rheology Andean orogeny crustal deformation deformation erosion finite element method flexure isostasy lithosphere numerical model plate tectonics rheology subduction zone viscoplasticity Andes South America |
dc.description.none.fl_txt_mv |
In this work, the modeling of plate tectonic processes associated with crustal deformation through a numerical framework for non-collisional Andean type orogens is presented. The main objectives of the numerical framework are to develop a numerical model in order to represent large-scale deformation in Andean type subduction zones, to include appropriate physical and mathematical laws that describe the behavior of the lithosphere, to model surface erosion taking into account dominant winds direction and the synorogenic topography of the orogen as the crustal erosion caused by friction between the subducting and the overriding plate and to include isostatic compensation behavior taking into account flexural rigidity. © 2005 Asociación Geológica Argentina. Fil:Quinteros, J. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Ramos, V.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Jacovkis, P.M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. |
description |
In this work, the modeling of plate tectonic processes associated with crustal deformation through a numerical framework for non-collisional Andean type orogens is presented. The main objectives of the numerical framework are to develop a numerical model in order to represent large-scale deformation in Andean type subduction zones, to include appropriate physical and mathematical laws that describe the behavior of the lithosphere, to model surface erosion taking into account dominant winds direction and the synorogenic topography of the orogen as the crustal erosion caused by friction between the subducting and the overriding plate and to include isostatic compensation behavior taking into account flexural rigidity. © 2005 Asociación Geológica Argentina. |
publishDate |
2005 |
dc.date.none.fl_str_mv |
2005 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 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://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p714_Quinteros |
url |
http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p714_Quinteros |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
http://creativecommons.org/licenses/by/2.5/ar |
dc.format.none.fl_str_mv |
application/pdf |
dc.source.none.fl_str_mv |
Rev. Asoc. Geol. Argent. 2005;60(4):714-723 reponame:Biblioteca Digital (UBA-FCEN) instname:Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales instacron:UBA-FCEN |
reponame_str |
Biblioteca Digital (UBA-FCEN) |
collection |
Biblioteca Digital (UBA-FCEN) |
instname_str |
Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales |
instacron_str |
UBA-FCEN |
institution |
UBA-FCEN |
repository.name.fl_str_mv |
Biblioteca Digital (UBA-FCEN) - Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales |
repository.mail.fl_str_mv |
ana@bl.fcen.uba.ar |
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1844618734068563968 |
score |
13.070432 |