Source: Journal of South American Earth Sciences. Unidade: IGC
Subjects: GEOCRONOLOGIA, PALEOPROTEROZOICO
ABNT
ÁVILA, Ciro Alexandre et al. Rhyacian (2.23–2.20 Ga)juvenile accretion in the southern São Francisco craton, Brazil: geochemical and isotopic evidence from the Serrinha magmatic suite, Mineiro belt. Journal of South American Earth Sciences, v. 29, n. 2, p. 464-482, 2010Tradução . . Disponível em: https://doi.org/10.1016/j.jsames.2009.07.009. Acesso em: 10 jun. 2024.APA
Ávila, C. A., Teixeira, W., Cordani, U. G., Moura, C. A., & Pereira, R. M. (2010). Rhyacian (2.23–2.20 Ga)juvenile accretion in the southern São Francisco craton, Brazil: geochemical and isotopic evidence from the Serrinha magmatic suite, Mineiro belt. Journal of South American Earth Sciences, 29( 2), 464-482. doi:10.1016/j.jsames.2009.07.009NLM
Ávila CA, Teixeira W, Cordani UG, Moura CA, Pereira RM. Rhyacian (2.23–2.20 Ga)juvenile accretion in the southern São Francisco craton, Brazil: geochemical and isotopic evidence from the Serrinha magmatic suite, Mineiro belt [Internet]. Journal of South American Earth Sciences. 2010 ; 29( 2): 464-482.[citado 2024 jun. 10 ] Available from: https://doi.org/10.1016/j.jsames.2009.07.009Vancouver
Ávila CA, Teixeira W, Cordani UG, Moura CA, Pereira RM. Rhyacian (2.23–2.20 Ga)juvenile accretion in the southern São Francisco craton, Brazil: geochemical and isotopic evidence from the Serrinha magmatic suite, Mineiro belt [Internet]. Journal of South American Earth Sciences. 2010 ; 29( 2): 464-482.[citado 2024 jun. 10 ] Available from: https://doi.org/10.1016/j.jsames.2009.07.009