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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Autores principales:	Quinteros, Javier, Ramos, Victor Alberto, Jacovkis, Pablo Miguel
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:	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v60_n4_p714_Quinteros http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p714_Quinteros
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

id	paper:paper_00044822_v60_n4_p714_Quinteros
record_format	dspace
spelling	paper:paper_00044822_v60_n4_p714_Quinteros2023-06-08T14:25:56Z Numerical modeling for the upper crustal deformation in the Southern Andes Quinteros, Javier Ramos, Victor Alberto Jacovkis, Pablo Miguel 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 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v60_n4_p714_Quinteros 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)
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, Javier Ramos, Victor Alberto Jacovkis, Pablo Miguel 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.
author	Quinteros, Javier Ramos, Victor Alberto Jacovkis, Pablo Miguel
author_facet	Quinteros, Javier Ramos, Victor Alberto Jacovkis, Pablo Miguel
author_sort	Quinteros, Javier
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	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v60_n4_p714_Quinteros http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p714_Quinteros
work_keys_str_mv	AT quinterosjavier numericalmodelingfortheuppercrustaldeformationinthesouthernandes AT ramosvictoralberto numericalmodelingfortheuppercrustaldeformationinthesouthernandes AT jacovkispablomiguel numericalmodelingfortheuppercrustaldeformationinthesouthernandes
_version_	1768546564405460992

Numerical modeling for the upper crustal deformation in the Southern Andes

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