Facies, microfacies, and diagenesis of late Callovian-early Oxfordian carbonates (La Manga Formation) in the West Central Argentinean high andes

At 32° 40′ south latitude the Andean orogen shows a typical thin-skinned fold and thrust belt that exposes the Mesozoic back-arc basin fill. The late Callovian - early Oxfordian limestones of the La Manga Formation were studied based on lithofacies, microfacies, and diagenetic processes in order to...

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Detalles Bibliográficos
Autores principales:	Lo Forte, G.L., Palma, R.M.
Formato:	JOUR
Materias:	Callovian carbonate system depositional environment diagenesis eustacy lithofacies microfacies Oxfordian Andes Argentina
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_08912556_v17_n1_p1_LoForte
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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