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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1997
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| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_05677505_v32_n1-2_p51_RodriguezFernandez http://hdl.handle.net/20.500.12110/paper_05677505_v32_n1-2_p51_RodriguezFernandez |
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