Convergent flow in a two-layer system and mountain building

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With the purpose of modeling the process of mountain building, we investigate the evolution of the ridge produced by the convergent motion of a system consisting of two layers of liquids that differ in density and viscosity to simulate the crust and the upper mantle that form a lithospheric plate. W...

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Detalles Bibliográficos
Autores principales:	Perazzo, C.A., Gratton, J.
Formato:	Artículo publishedVersion
Publicado:	2010
Materias:	Basal tractions Lithospheric Mountain belts Mountain building Nonlinear differential equation Self-similar solution Theoretical result Two layers Two-layer systems Upper mantle Differential equations Landforms Nonlinear equations Density of liquids
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_10706631_v22_n5_p1_Perazzo https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_10706631_v22_n5_p1_Perazzo_oai
Aporte de:	Repositorio Digital de la Universidad de Buenos Aires (UBA) de Universidad de Buenos Aires

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