1.
Llambías EJ, Leanza HA, Carbone O. Tectono-magmatic evolution during the Permian to the Early Jurassic in the Cordillera del Viento (37°05´S - 37°15´S): new geological and geochemical evidences for the early stages of the Neuquén basin. RAGA [Internet]. 2007Jun.30 [cited 2024Apr.16];62(2):217-35. Available from: https://revista.geologica.org.ar/raga/article/view/1118