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
Autores principales: Pose, F.A., Spagnuolo, M., Folguera, A.
Formato: JOUR
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: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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