Stratigraphy and structure of the Argentine Central Andes between 30°and 31°S latitude

In a cross-section through the Argentine central Andes, two large groups of rocks can be distinguished: a Gondwanic (Paleozoic) basement, and an Andean cover. The basement is constituted by marine sedimentary units, intruded by Upper Paleozoic granitoid rocks. The most important Gondwanic structures...

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Autores principales: Rodríguez Fernández, L.R., Heredia, N., Espina, R.G., Cegarra, M.I.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_05677505_v32_n1-2_p51_RodriguezFernandez
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