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:
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00401951_v628_n_p228_Prezzi
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