Numerical modeling for the upper crustal deformation in the Southern Andes
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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I28-R145-paper_00044822_v60_n4_p714_Quinteros_oai2024-08-16 Quinteros, J. Ramos, V.A. Jacovkis, P.M. 2005 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. application/pdf http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p714_Quinteros info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar Rev. Asoc. Geol. Argent. 2005;60(4):714-723 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 Numerical modeling for the upper crustal deformation in the Southern Andes info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v60_n4_p714_Quinteros_oai |
| institution |
Universidad de Buenos Aires |
| institution_str |
I-28 |
| repository_str |
R-145 |
| collection |
Repositorio Digital de la Universidad de Buenos Aires (UBA) |
| 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 https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v60_n4_p714_Quinteros_oai |
| work_keys_str_mv |
AT quinterosj numericalmodelingfortheuppercrustaldeformationinthesouthernandes AT ramosva numericalmodelingfortheuppercrustaldeformationinthesouthernandes AT jacovkispm numericalmodelingfortheuppercrustaldeformationinthesouthernandes |
| _version_ |
1809356945695440896 |