Middle slope contourite deposits and associated sedimentary facies off NE Argentina

The Argentine continental margin is characterised by a large contourite depositional system driven by southern-sourced water masses flowing at different water depths. Interest in contourite deposits is increasing in geoscience and related fields, though knowledge of the Argentine contourite system i...

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Detalles Bibliográficos
Autores principales:	Bozzano, G., Violante, R.A., Cerredo, M.E.
Formato:	JOUR
Materias:	Argentina Climate condition Continental margin Contourite depositional systems Depth range Geosciences Key factors Late Pleistocene-Holocene Patagonia Sediment source areas Sedimentary facies Sedimentary process Water depth Water mass Anoxic sediments Deposits Gravel Magnetic susceptibility Sea level Sedimentology Process control continental margin deposition facies grain size petrography Pleistocene-Holocene boundary sea level slope water depth water mass
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_02760460_v31_n5-6_p495_Bozzano
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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