Evolution of the upper crustal deformation in subduction zones

The 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....

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Detalles Bibliográficos
Autores principales:	Quinteros, J., Jacovkis, P.M., Ramos, V.A.
Formato:	JOUR
Materias:	Erosion Finite element method Mathematical models Plates (structural components) Stress analysis Tectonics Velocity Andean system Crustal deformation Mechanical behavior Tectonic stresses Shear deformation
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00218936_v73_n6_p984_Quinteros
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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