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- W2912651476 abstract "Les « distributive fluvial systems »(DFS) sont d’importants elements geomorphologiques pouvant dominer les systemes de deposition dans les milieux continentaux aggradants actuels. Par analogie, ces systemes seraient aussi predominants dans les anciennes successions sedimentaires. L’etude presentee ici se concentre sur le developpement du bassin d’avant-pays de Cacheuta (Province de Mendoza, Argentine) lors du Miocene, le secteur sud du systeme d’avant-pays andeen. La succession stratigraphique etudiee est constituee des formations continentales Marino et La Pilona, ayant enregistre les principales phases d’exhumation de la Cordillere des Andes dans la region. Cette etude presente l’utilisation combinee de methodes analytiques quantitatives et d’observations sur la sedimentologie des depots. Le but etant de comprendre l’effet des facteurs de forcage allogeniques ainsi que des processus purement autogeniques dans la composition des gres provenant des chenaux fluviatiles, cela dans un contexte de progradation d’un systeme de cone fluviatile." @default.
- W2912651476 created "2019-02-21" @default.
- W2912651476 creator A5018130790 @default.
- W2912651476 date "2018-01-01" @default.
- W2912651476 modified "2023-09-23" @default.
- W2912651476 title "Genesis and evolution of a foreland fluvial-fan and aeolian succession: a high-resolution multiproxy study of the Miocene Cacheuta basin infill, Mendoza (Argentina)" @default.
- W2912651476 doi "https://doi.org/10.13097/archive-ouverte/unige:113186" @default.
- W2912651476 hasPublicationYear "2018" @default.
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