Geochemistry and petrology of a Middle Tithonian limestone-marl rhythmite in the Neuquén Basin, Argentina: Depositional and burial history

The Middle Tithonian Los Catutos Member (Vaca Muerta Formation, Neuquén Basin), is lithologically and geochemically similar to limestone-marl alternations from the Late Jurassic of the northern hemisphere. Both marls and limestones are pelbiomicrites and biopelmicrites principally composed of pellet...

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Autores principales: Scasso, R.A., Alonso, M.S., Lanés, S., Villar, H.J., Laffitte, G.
Formato: SER
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_03058719_v252_n_p207_Scasso
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