Flexural isostasy in the Bolivian Andes: Chaco foreland basin development

The Chaco foreland basin was initiated during the late Oligocene as a result of thrusting in the Eastern Cordillera in response to Nazca-South America plate convergence. Foreland basins are the result of the flexural isostatic response of an elastic plate to orogenic and/or thrust sheet loading. We...

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Detalles Bibliográficos
Autores principales:	Prezzi, C.B., Uba, C.E., Götze, H.-J.
Formato:	JOUR
Materias:	Basin development Central Andes Chaco foreland Flexural isostasy Flexural modelling Geodesy Plates (structural components) Sedimentology Tectonics basin evolution elastic property foreland basin gravity anomaly isostasy Moho Oligocene thrust Andes South America
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00401951_v474_n3-4_p526_Prezzi
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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