Convergent flow in a two-layer system and plateau development

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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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Detalles Bibliográficos
Autores principales: Gratton, J., Perazzo, C.A.
Formato: JOUR
Materias:
Approximate formulas
Liquid layer
Lithospheric
Mountain ranges
Nonlinear differential equation
Traveling wave
Two layer model
Two-layer systems
Upper mantle
Approximation algorithms
Differential equations
Liquids
Viscosity
Nonlinear equations
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_10706631_v23_n4_p_Gratton
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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