dc.creatorQuinteros, Javier
dc.creatorJacovkis, Pablo Miguel
dc.creatorRamos, Victor Alberto
dc.date.accessioned2020-01-07T15:21:38Z
dc.date.accessioned2022-10-15T03:59:07Z
dc.date.available2020-01-07T15:21:38Z
dc.date.available2022-10-15T03:59:07Z
dc.date.created2020-01-07T15:21:38Z
dc.date.issued2006-11
dc.identifierQuinteros, Javier; Jacovkis, Pablo Miguel; Ramos, Victor Alberto; Evolution of the upper crustal deformation in subduction zones; American Society of Mechanical Engineers; Journal Of Applied Mechanics-transactions Of The Asme; 73; 6; 11-2006; 984-994
dc.identifier0021-8936
dc.identifierhttp://hdl.handle.net/11336/93766
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4342946
dc.description.abstractThe uplift and evolution of a noncollisional orogen developed along a subduction zone, such as the Andean system, is a direct consequence of the interrelation between plate tectonic stresses and erosion. Tectonic stresses are related to the convergence velocity and thermal state, among other causes. In this paper, a new model designed to investigate the evolution of the topography and the upper crustal deformation of noncollisional orogens in a subduction zone produced by the oceanic crust being subducted is presented. The mechanical behavior of the crust was modeled by means of finite elements methods to solve Stokes equations for a strain-rate-dependent viscoplastic rheology. The model takes into account erosion effects using interface-tracking methods to assisn fictitious properties to nonmaterial elements.
dc.languageeng
dc.publisherAmerican Society of Mechanical Engineers
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/https://doi.org/10.1115/1.2204962
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://asmedigitalcollection.asme.org/appliedmechanics/article-abstract/73/6/984/465599/Evolution-of-the-Upper-Crustal-Deformation-in
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.subjectfinite element
dc.subjectStokes equations
dc.subjectviscoplastic rheology
dc.subjectsubduction zones
dc.titleEvolution of the upper crustal deformation in subduction zones
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:ar-repo/semantics/artículo
dc.typeinfo:eu-repo/semantics/publishedVersion


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