Convergent flow in a two-layer system and mountain building

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: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_10706631_v22_n5_p1_Perazzo
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