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  1. 1
    Saprophytic fungi in upper permian ferns from Paraguay /

    Saprophytic fungi in upper permian ferns from Paraguay / by Lutz, Alicia I.

    Published 1992
    Book
  2. 2
    Estudio anatómico de una nueva Lycopsida del Pérmico de Bolivia

    Estudio anatómico de una nueva Lycopsida del Pérmico de Bolivia by Archangelsky, Sergio, De la Sota, Elías

    Published 2023
    Subjects: “…Paleobotany; Lycopsida; Bolivia; Permian;…”
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    info:eu-repo/semantics/article
  3. 3
    Failure Modes in Road Tunnels of Sierra Valle Fertil. San Juan. Argentina

    Failure Modes in Road Tunnels of Sierra Valle Fertil. San Juan. Argentina by Aceituno Cieri, Paula, Martino, Roberto D., Giambastiani, Mauricio, Rocca, Ricardo J.

    Published 2023
    Subjects:
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  4. 4
    Nuevos polysperms glossopterid de la Formación del Pérmico La Golondrina (Provincia de Santa Cruz, Argentina): afinidades y potenciales implicaciones biostratigráficas

    Nuevos polysperms glossopterid de la Formación del Pérmico La Golondrina (Provincia de Santa Cruz, Argentina): afinidades y potenciales implicaciones biostratigráficas by Cariglino, Bárbara

    “…New glossopterid polysperms from the Permian La Golondrina Formation (Santa Cruz Province, Argentina): Potential affinities and biostratigraphic implications…”
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    Article
  5. 5
    Nuevos fósiles de madera de gimnosperma, una estructura de semilla-óvulo y una nueva afinidad genérica con Cedroxylon canoasense Rau del Pérmico y Triásico-Jurásico del Sur de Brasil.

    Nuevos fósiles de madera de gimnosperma, una estructura de semilla-óvulo y una nueva afinidad genérica con Cedroxylon canoasense Rau del Pérmico y Triásico-Jurásico del Sur de Bras... by Crisafulli, Alexandra

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    Article
  6. 6
    THE UPPER PALEOZOIC IN THE RIO SECO DE LA INVERNADA. SAN JUAN.

    THE UPPER PALEOZOIC IN THE RIO SECO DE LA INVERNADA. SAN JUAN. by Caballe, Marcelo F., Furque, Guillermo

    Published 2023
    “…The paper describes a sedimentary sequence (Carrizo Formation ) of the Upper Paleozoic outcropping in the valley of rio Seco de la Invernada, within the environment of the central Precordillera of San Juan.The sequence, 529m thick, is made up of a basal psamitic unit of eolian origen, a mostly pelitic unit considered to be lacustrine, and two uppermost units of sandstones, conglomerates and shales, whose origen is ascribed to rivers of moderate to high sinuosity.Some basaltic to rhyolitic sills are intercalated in the sequence.On the basis of a possible relationship with sedimentary rocks of the Ojo de Agua Formation, the age of the sequence is referred to the Permian s. l.…”
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    info:eu-repo/semantics/article

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