Source: Journal of South American Earth Sciences. Unidade: IGC
Subjects: CRÁTON, ENXAME DE DIQUES, ISÓTOPOS, PETROLOGIA
ABNT
GIOVANARDI, Tommaso et al. Mafic dyke swarms at 1882, 535 and 200Ma in the Carajás region, Amazonian Craton: Sr Nd isotopy, trace element geochemistry and inferences on their origin and geological settings. Journal of South American Earth Sciences, v. 92, n. , p. 197-208, 2019Tradução . . Disponível em: https://doi.org/10.1016/j.jsames.2019.02.017. Acesso em: 25 set. 2024.APA
Giovanardi, T., Girardi, V. A. V., Teixeira, W., & Mazzucchelli, M. (2019). Mafic dyke swarms at 1882, 535 and 200Ma in the Carajás region, Amazonian Craton: Sr Nd isotopy, trace element geochemistry and inferences on their origin and geological settings. Journal of South American Earth Sciences, 92( ), 197-208. doi:10.1016/j.jsames.2019.02.017NLM
Giovanardi T, Girardi VAV, Teixeira W, Mazzucchelli M. Mafic dyke swarms at 1882, 535 and 200Ma in the Carajás region, Amazonian Craton: Sr Nd isotopy, trace element geochemistry and inferences on their origin and geological settings [Internet]. Journal of South American Earth Sciences. 2019 ; 92( ): 197-208.[citado 2024 set. 25 ] Available from: https://doi.org/10.1016/j.jsames.2019.02.017Vancouver
Giovanardi T, Girardi VAV, Teixeira W, Mazzucchelli M. Mafic dyke swarms at 1882, 535 and 200Ma in the Carajás region, Amazonian Craton: Sr Nd isotopy, trace element geochemistry and inferences on their origin and geological settings [Internet]. Journal of South American Earth Sciences. 2019 ; 92( ): 197-208.[citado 2024 set. 25 ] Available from: https://doi.org/10.1016/j.jsames.2019.02.017