Convergent flow in a two-layer system and plateau development

In order to describe the development of plateaus such as the Tibet and the Altiplano we extend the two-layer model used in a previous paper [C. A. Perazzo and J. Gratton, Phys. Fluids22, 056603 (2010)] to reproduce the evolution of mountain ranges. As before, we consider the convergent motion of a s...

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Autores principales: Gratton, Julio, Perazzo, Carlos Alberto
Publicado: 2011
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_10706631_v23_n4_p_Gratton
http://hdl.handle.net/20.500.12110/paper_10706631_v23_n4_p_Gratton
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