Model for Andean orogenic volume variation and shortening in the 20°-46°S sector

The orogenic volume of the Andes is the result of the equilibrium between the tectonic uplift and erosion. The different rates of shortening along the western margin of the South American continent have defined contrasting morphostructural settings. The orogenic volume along the southern Central And...

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Detalles Bibliográficos
Publicado:	2005
Materias:	Andes Climatic control Orogenic volume Shortening Strain partitioning Andean orogeny continental margin crustal shortening empirical analysis erosion isostasy latitudinal gradient model morphostructure slab strain partitioning subduction uplift volume change Patagonia South America
Acceso en línea:	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v60_n4_p724_Pose http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p724_Pose
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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