Skip navigation
Skip navigation

Sedimentology, palaeobotany and geochronology of the Piedra del Aguila Formation (Lower Jurassic, Neuquen) [Consideraciones acerca de la sedimentologia, paleobotanica y geocronologia de la Formacion Piedra del Aguila (Jurasico Inferior, Neuquan)]

Spalletti, L.A.; Franzese, Juan; Morel, Eduardo; D'Elia, Leandro; Zuniga, Adolfo; Fanning, Christopher


At its type locality, the Piedra del Águila Formation is a 71.6 m thick homoclinal succession that lies on a weathering palaeosurface developed on the igneous-metamorphic basement (Mamil Choique Formation), and is unconformably covered by the Lower Juras

CollectionsANU Research Publications
Date published: 2010
Type: Journal article
Source: Revista de la Asociacion Geologica Argentina


File Description SizeFormat Image
01_Spalletti_Sedimentology,_palaeobotany_2010.pdf508.65 kBAdobe PDF    Request a copy

Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.

Updated:  17 November 2022/ Responsible Officer:  University Librarian/ Page Contact:  Library Systems & Web Coordinator