Assuntos: ROCHAS ALCALINAS, PETROGRAFIA, QUÍMICA MINERAL, DIFRAÇÃO POR RAIOS X, GEOQUÍMICA
ABNT
SOUZA, Amanda Andrade de et al. Genesis of Fe-Ti-(V) oxide-rich rocks by open-system evolution of mafic alkaline magmas: the case of the Ponte Nova Massif, SE Brazil. Minerals, v. 14, n. , p. 724-, 2024Tradução . . Disponível em: https://doi.org/10.3390/min14070724. Acesso em: 10 nov. 2025.APA
Souza, A. A. de, Azzone, R. G., Chmyz, L., Cetina, L., Andrade, F. R. D. de, Martins, J. V., et al. (2024). Genesis of Fe-Ti-(V) oxide-rich rocks by open-system evolution of mafic alkaline magmas: the case of the Ponte Nova Massif, SE Brazil. Minerals, 14( ), 724-. doi:10.3390/min14070724NLM
Souza AA de, Azzone RG, Chmyz L, Cetina L, Andrade FRD de, Martins JV, Ruberti E, Gomes CB. Genesis of Fe-Ti-(V) oxide-rich rocks by open-system evolution of mafic alkaline magmas: the case of the Ponte Nova Massif, SE Brazil [Internet]. Minerals. 2024 ; 14( ): 724-.[citado 2025 nov. 10 ] Available from: https://doi.org/10.3390/min14070724Vancouver
Souza AA de, Azzone RG, Chmyz L, Cetina L, Andrade FRD de, Martins JV, Ruberti E, Gomes CB. Genesis of Fe-Ti-(V) oxide-rich rocks by open-system evolution of mafic alkaline magmas: the case of the Ponte Nova Massif, SE Brazil [Internet]. Minerals. 2024 ; 14( ): 724-.[citado 2025 nov. 10 ] Available from: https://doi.org/10.3390/min14070724
