Sequential development of tidal ravinement surfaces in macro- to hypertidal estuaries with high volcaniclastic input: the Miocene Puerto Madryn Formation (Patagonia, Argentina)

The late Miocene beds of the Puerto Madryn Formation (Provincia del Chubut, Argentina) are formed by shallow marine and estuarine sediments. The latter include several tidal-channel infills well exposed on the cliffy coast of the Peninsula Valdés. The Bahía Punta Fósil and Cerro Olazábal paleochanne...

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Detalles Bibliográficos
Autores principales:	Scasso, R.A., Cuitiño, J.I.
Formato:	JOUR
Materias:	Erosion Ocean currents Saline water Sedimentation Sediments Tidal power Volcanoes Channel migration Erosion surfaces Estuarine sediments Fluvial process Sediment supply Sedimentation rates Volcanic eruptions Volcaniclastics Estuaries bioclastic rock conglomerate depositional environment depositional sequence estuarine environment estuarine sediment Miocene paleochannel sedimentation rate sequence stratigraphy shallow water transgression volcaniclastic deposit Argentina Chubut Patagonia
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_02760460_v37_n4_p427_Scasso
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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