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  1. 1
    Findings of intraformational striated pavements in the late carboniferous glacial deposits of the Andean Precordillera, Argentina

    Findings of intraformational striated pavements in the late carboniferous glacial deposits of the Andean Precordillera, Argentina by Pablo J. Alonso Muruaga, Carlos O. Limarino, Luis A. Spalletti, Ferrán Colombo Piñol, Pablo Juárez

    Published 2011-12-01
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  2. 2
    Findings of intraformational striated pavements in the late carboniferous glacial deposits of the Andean Precordillera, Argentina

    Findings of intraformational striated pavements in the late carboniferous glacial deposits of the Andean Precordillera, Argentina by Pablo J. Alonso Muruaga, Carlos O. Limarino, Luis A. Spalletti, Ferrán Colombo Piñol, Pablo Juárez

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  3. 3
    Findings of intraformational striated pavements in the late carboniferous glacial deposits of the Andean Precordillera, Argentina

    Findings of intraformational striated pavements in the late carboniferous glacial deposits of the Andean Precordillera, Argentina by Pablo J. Alonso Muruaga, Carlos O. Limarino, Luis A. Spalletti, Ferrán Colombo Piñol, Pablo Juárez

    Published 2021-03-01
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    Article
  4. 4
    Findings of intraformational striated pavements in the late carboniferous glacial deposits of the Andean Precordillera, Argentina

    Findings of intraformational striated pavements in the late carboniferous glacial deposits of the Andean Precordillera, Argentina by Pablo J. Alonso Muruaga, Carlos O. Limarino, Luis A. Spalletti, Ferrán Colombo Piñol, Pablo Juárez

    Published 2021-03-01
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  5. 5
    Procesos gravitacionales-fluviales y preservación de vegetación boscosa en un área volcánica: Formación Rancahué (Oligoceno), Andes neuquinos, Argentina

    Procesos gravitacionales-fluviales y preservación de vegetación boscosa en un área volcánica: Formación Rancahué (Oligoceno), Andes neuquinos, Argentina by Luis A. Spalletti, Gonzalo D. Veiga, Juan R. Franzese

    Published 2013-09-01
    “…Andean Geology…”
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  6. 6
    Variability of continental depositional systems during lowstand sedimentation: an example from the Kimmeridgian of the Neuquen Basin, Argentina

    Variability of continental depositional systems during lowstand sedimentation: an example from the Kimmeridgian of the Neuquen Basin, Argentina by Luis A. Spalletti, Gonzalo D. Veiga

    “…The Kimmeridgian lowstand wedge was developed slightly after the emergence of the Andean magmatic arc and the tectonic inversion of previous intrabasinal extensional structures. …”
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  7. 7
    Variability of continental depositional systems during lowstand sedimentation: an example from the Kimmeridgian of the Neuquen Basin, Argentina

    Variability of continental depositional systems during lowstand sedimentation: an example from the Kimmeridgian of the Neuquen Basin, Argentina by Luis A. Spalletti, Gonzalo D. Veiga

    Published 2021-03-01
    “…The Kimmeridgian lowstand wedge was developed slightly after the emergence of the Andean magmatic arc and the tectonic inversion of previous intrabasinal extensional structures. …”
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    Article
  8. 8
    Variability of continental depositional systems during lowstand sedimentation: an example from the Kimmeridgian of the Neuquen Basin, Argentina

    Variability of continental depositional systems during lowstand sedimentation: an example from the Kimmeridgian of the Neuquen Basin, Argentina by Luis A. Spalletti, Gonzalo D. Veiga

    Published 2021-03-01
    “…The Kimmeridgian lowstand wedge was developed slightly after the emergence of the Andean magmatic arc and the tectonic inversion of previous intrabasinal extensional structures. …”
    Get full text
    Article
  9. 9
    Variability of continental depositional systems during lowstand sedimentation: an example from the Kimmeridgian of the Neuquen Basin, Argentina

    Variability of continental depositional systems during lowstand sedimentation: an example from the Kimmeridgian of the Neuquen Basin, Argentina by Luis A. Spalletti, Gonzalo D. Veiga

    Published 2007-12-01
    “…The Kimmeridgian lowstand wedge was developed slightly after the emergence of the Andean magmatic arc and the tectonic inversion of previous intrabasinal extensional structures. …”
    Get full text
    Article

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