Numerical modeling for the upper crustal deformation in the Southern Andes

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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...

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Autores principales: Quinteros, J., Ramos, V.A., Jacovkis, P.M.
Formato: Artículo publishedVersion
Lenguaje:Inglés
Publicado: 2005
Materias:
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
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p714_Quinteros
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Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires
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spelling paperaa:paper_00044822_v60_n4_p714_Quinteros2023-06-12T16:40:08Z Numerical modeling for the upper crustal deformation in the Southern Andes Rev. Asoc. Geol. Argent. 2005;60(4):714-723 Quinteros, J. Ramos, V.A. Jacovkis, P.M. 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 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. 2005 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion application/pdf eng info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p714_Quinteros
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
language Inglés
orig_language_str_mv eng
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
spellingShingle 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
Quinteros, J.
Ramos, V.A.
Jacovkis, P.M.
Numerical modeling for the upper crustal deformation in the Southern Andes
topic_facet 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
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.
format Artículo
Artículo
publishedVersion
author Quinteros, J.
Ramos, V.A.
Jacovkis, P.M.
author_facet Quinteros, J.
Ramos, V.A.
Jacovkis, P.M.
author_sort Quinteros, J.
title Numerical modeling for the upper crustal deformation in the Southern Andes
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
publishDate 2005
url http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p714_Quinteros
work_keys_str_mv AT quinterosj numericalmodelingfortheuppercrustaldeformationinthesouthernandes
AT ramosva numericalmodelingfortheuppercrustaldeformationinthesouthernandes
AT jacovkispm numericalmodelingfortheuppercrustaldeformationinthesouthernandes
_version_ 1769810061520011264

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