Source: Journal of South American Earth Science. Unidade: IGC
Subjects: GEOCRONOLOGIA, VULCANISMO
ABNT
GONZÁLEZ, Santiago Nicolás et al. Middle Triassic trachytic lava flows associated with coeval dyke swarm in the North Patagonian Massif: a postorogenic magmatism related to extensional collapse of the Gondwanide orogen. Journal of South American Earth Science, v. 75, p. 134–143, 2017Tradução . . Disponível em: https://doi.org/10.1016/j.jsames.2017.02.007. Acesso em: 30 ago. 2024.APA
González, S. N., Greco, G. A., Sato, A. M., Llambías, E. J., Basei, M. A. S., González, P. D., & Díaz, P. E. (2017). Middle Triassic trachytic lava flows associated with coeval dyke swarm in the North Patagonian Massif: a postorogenic magmatism related to extensional collapse of the Gondwanide orogen. Journal of South American Earth Science, 75, 134–143. doi:10.1016/j.jsames.2017.02.007NLM
González SN, Greco GA, Sato AM, Llambías EJ, Basei MAS, González PD, Díaz PE. Middle Triassic trachytic lava flows associated with coeval dyke swarm in the North Patagonian Massif: a postorogenic magmatism related to extensional collapse of the Gondwanide orogen [Internet]. Journal of South American Earth Science. 2017 ; 75 134–143.[citado 2024 ago. 30 ] Available from: https://doi.org/10.1016/j.jsames.2017.02.007Vancouver
González SN, Greco GA, Sato AM, Llambías EJ, Basei MAS, González PD, Díaz PE. Middle Triassic trachytic lava flows associated with coeval dyke swarm in the North Patagonian Massif: a postorogenic magmatism related to extensional collapse of the Gondwanide orogen [Internet]. Journal of South American Earth Science. 2017 ; 75 134–143.[citado 2024 ago. 30 ] Available from: https://doi.org/10.1016/j.jsames.2017.02.007