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)]
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Spalletti, L.A.
Franzese, Juan
Morel, Eduardo
D'Elia, Leandro
Zuniga, Adolfo
Fanning, Christopher
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Asociacion Geologica Argentina
Abstract
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
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Revista de la Asociacion Geologica Argentina
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Restricted until
2037-12-31