Palaeoenvironmental significance of middle Oxfordian deep marine deposits from La Manga Formation, Neuquén Basin, Argentina

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The Callovian-Oxfordian of the Neuquén Basin (Argentina) is characterized by an extensive marine carbonate system (La Manga Formation) with a predominance of shallow and middle ramp deposits, although locally in tectonically controlled settings, deeper deposits also formed. These middle Oxfordian de...

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Detalles Bibliográficos
Autores principales:	Palma, R.M., Bressan, G.S., Kietzmann, D.A., Riccardi, A.C., Martín-Chivelet, J., López- Gómez, J.
Formato:	JOUR
Materias:	Cylostratigraphy Hemipelagic Middle Oxfordian Neuquén Basin TOC carbonate sediment deep sea fossil record marine sediment Oxfordian paleoenvironment subsidence Argentina Neuquen Basin
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_16986180_v40_n3_p507_Palma
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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