Using fluvial cyclicity to decipher the interaction of basement- and fold-thrust-belt tectonics in a broken foreland basin: Vinchina Formation (Miocene), northwestern Argentina

The Miocene Vinchina Formation is made up of more than 5100 meters of siliciclastic sediments deposited mostly in fluvial environments in a broken foreland basin without any connection with the sea during a period of arid to semiarid climatic conditions. Repetitive changes in fluvial facies allow th...

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Autores principales: Marenssi, S.A., Ciccioli, P.L., Limarino, C.O., Schencman, L.J., Diaz, M.Y.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_15271404_v85_n4_p361_Marenssi
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