The Triassic-Jurassic boundary in the Andes of Argentina

The Arroyo Malo Formation at Alumbre Creek, on the northern bank of the Atuel River, west central Argentina, comprises a c. 300 m thick continuous marine succession across the Triassic-Jurassic System boundary, consisting of massive and laminated pelites indicative of a slope depositional environmen...

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Autores principales: Riccardi, Alberto Carlos, Damborenea, Susana Ester, Manceñido, Miguel Oscar, Iglesia Llanos, María Paula
Formato: Articulo
Lenguaje:Inglés
Publicado: 2004
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Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/97245
https://ri.conicet.gov.ar/11336/81386
https://riviste.unimi.it/index.php/RIPS/article/view/6266
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