Fonte: Journal of South American Earth Sciences. Unidade: IGC
Assuntos: PETROLOGIA ÍGNEA, MAGMA
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AZZONE, Rogério Guitarrari et al. Trace element composition of parental magmas from mafic–ultramafic cumulates determined by in situ mineral analyses: the Juquiá mafic–ultramafic alkaline–carbonatite massif, SE Brazil. Journal of South American Earth Sciences, v. 41, p. ¦ 5-21, 2013Tradução . . Disponível em: https://doi.org/10.1016/j.jsames.2012.07.005. Acesso em: 06 nov. 2024.APA
Azzone, R. G., Enrich Rojas, G. E., Gomes, C. B., & Ruberti, E. (2013). Trace element composition of parental magmas from mafic–ultramafic cumulates determined by in situ mineral analyses: the Juquiá mafic–ultramafic alkaline–carbonatite massif, SE Brazil. Journal of South American Earth Sciences, 41, ¦ 5-21. doi:10.1016/j.jsames.2012.07.005NLM
Azzone RG, Enrich Rojas GE, Gomes CB, Ruberti E. Trace element composition of parental magmas from mafic–ultramafic cumulates determined by in situ mineral analyses: the Juquiá mafic–ultramafic alkaline–carbonatite massif, SE Brazil [Internet]. Journal of South American Earth Sciences. 2013 ; 41¦ 5-21.[citado 2024 nov. 06 ] Available from: https://doi.org/10.1016/j.jsames.2012.07.005Vancouver
Azzone RG, Enrich Rojas GE, Gomes CB, Ruberti E. Trace element composition of parental magmas from mafic–ultramafic cumulates determined by in situ mineral analyses: the Juquiá mafic–ultramafic alkaline–carbonatite massif, SE Brazil [Internet]. Journal of South American Earth Sciences. 2013 ; 41¦ 5-21.[citado 2024 nov. 06 ] Available from: https://doi.org/10.1016/j.jsames.2012.07.005