Petrology and geochemistry of a limestone-marl rhythmite from the Southern Hemisphere: The Los Catutos Member (Vaca Muerta Formation). Middle Tithonian of Neuquén Basin

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A 25 m thick, rhythmic, limestone-marl alternation of Los Catutos Member (Vaca Muerta Formation, Neuquén Basin), was studied bed by hed in several quarries near Zapala. Beds up to 1 m thick are of massive or laminated, lithographic, fossiliferous limestone, locally mottled or weakly bioturbated (?Ch...

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Detalles Bibliográficos
Autores principales: Scasso, R.A., Alonso, M.S., Lanés, S., Villar, H.J., Lippai, H.
Formato: Artículo publishedVersion
Publicado: 2002
Materias:
Cyclicity
Geochemistry
Limestone
Neuquen Basin
Rhytmite
Stable isotopes
Upper Jurassic
cyclic sedimentation
depositional environment
Jurassic
limestone
marl
rhythmite
Tithonian
Argentina
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00044822_v57_n2_p143_Scasso
https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v57_n2_p143_Scasso_oai
Aporte de:
Repositorio Digital de la Universidad de Buenos Aires (UBA) de Universidad de Buenos Aires

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