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- W2105216711 abstract "Tectono-magmatic evolution during the Permian to the Early Jurassic in the Cordillera del Viento (37°05´S - 37°15´S): new geological and geoche- mical evidences for the early stages of the Neuquen basin. The southern extremity of the Cordillera del Viento is mainly composed of volcanic sequences, which form the basement of the Neuquen basin. The oldest rocks are the sediments in the Huaraco Formation, Andacollo Group, of Upper Carboniferous age. After being folded by the San Rafael orogenic phase during the Lower Permian, these sediments were intruded by granodioritic and monzogranitic plutons along with dikes and domes of rhyolitic nature. They were then covered in angular unconformity by rhyolitic ignimbrites, which are co-" @default.
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- W2105216711 date "2007-01-06" @default.
- W2105216711 modified "2023-09-24" @default.
- W2105216711 title "EVOLUCIÓN TECTONO-MAGMÁTICA DURANTE EL PÉRMICO AL JURÁSICO TEMPRANO EN LA CORDILLERA DEL VIENTO (37°05´S - 37°15´S): NUEVAS EVIDENCIAS GEOLÓGICAS Y GEOQUÍMICAS DEL INICIO DE LA CUENCA NEUQUINA" @default.
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