Peritidal cyclic sedimentation from La Manga Formation (Oxfordian), Neuquén Basin, Mendoza, Argentina

The La Manga Formation consists of marine carbonates and represents most of the sedimentary record of the Callovian-Oxfordian in the Neuquén Basin. Three localities in the southern Mendoza province were studied and their cyclicity was determined by means of facies analysis and their vertical arrange...

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Detalles Bibliográficos
Autores principales: Palma, R.M., Kietzmann, D.A., Bressan, G.S., Martín-Chivelet, J., López-Gómez, J., Farias, M.E., Iglesias Llanos, M.P.
Formato: JOUR
Materias:
Carbonate ramp
Fischer plots
Jurassic
Peritidal cycles
breccia
Callovian
carbonate ramp
carbonate sediment
conglomerate
cyclicity
facies analysis
Oxfordian
sedimentation
shallow water
tidal cycle
Argentina
Mendoza
Neuquen Basin
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_08959811_v47_n_p1_Palma
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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