Evolution of the Paleozoic Claromecó Basin (Argentina) and geodynamic implications for the southwestern margin of Gondwana: Insights from isostatic, gravimetric and magnetometric models

The evolution of the Paleozoic Claromecó Basin is intimately related to contemporaneous tectonic events in the Sierras Australes and Patagonia (Argentina). These deformation and tectonomagmatic processes record, in turn, the evolution of the southwestern margin of Gondwana during the Paleozoic, whic...

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Detalles Bibliográficos
Autores principales: Prezzi, C.B., Vizán, H., Vázquez, S., Renda, E., Oriolo, S., Japas, M.S.
Formato: JOUR
Materias:
Deformation
Geodynamics
Patagonia
Sierras Australes
Subsidence
Geochronology
Piles
Tectonics
Accommodation space
Back-arc extensions
Basin evolution
Dynamic subsidences
Possible mechanisms
Subduction process
backarc basin
basin evolution
deformation
extensional tectonics
geodynamics
Gondwana
gravimetry
isostasy
magnetometer
Paleozoic
subsidence
Argentina
Buenos Aires [Argentina]
Claromeco Basin
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00401951_v742-743_n_p120_Prezzi
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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