Andean foreland evolution and flexure in NW Argentina: Chaco-Paraná Basin

The Chaco-Paraná Basin was initiated during the late Oligocene as a result of shortening in response to Nazca-South America plate convergence, which produced a fold and thrust belt in the backarc region of the Central Andes. Foreland basins are the result of the flexural isostatic response of an ela...

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Detalles Bibliográficos
Autores principales: Prezzi, C.B., Götze, H.-J., Schmidt, S.
Formato: JOUR
Materias:
Basin development
Central Andes
Chaco-Paraná Basin
Flexural modeling
Geodynamics
Plates (structural components)
Sedimentology
Eastern Cordillera
Elastic thickness
Fold-and-thrust belts
Gravity anomalies
Plate convergence
Spatiotemporal evolution
Late Oligocene
Tectonics
crustal shortening
flexure
fold and thrust belt
foreland basin
Oligocene
plate convergence
plate motion
tectonic evolution
tectonic setting
Andean orogeny
basin evolution
geodynamics
Nazca plate
sediment thickness
three-dimensional modeling
Andes
Argentina
Chaco [Argentina]
Parana Basin
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00401951_v628_n_p228_Prezzi
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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