Source: Eos Transactions AGU, v.91, n.26, Meeting of the Americas Supplement, abstract V21B-02, 2010. Conference titles: 2010 Meeting of the Americas. Unidade: IAG
Subjects: GEOQUÍMICA, MAGMATISMO, ISÓTOPOS, ÓSMIO, MANTO DA TERRA (PROCESSOS)
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ROCHA JÚNIOR, Eduardo Reis Viana et al. Osmium isotope and highly siderophile element systematics of the Paraná Flood Basalt Province: implications for mantle sources. 2010, Anais.. Washington: American Geophysical Union, 2010. . Acesso em: 31 out. 2024.APA
Rocha Júnior, E. R. V., Marques, L. S., Walker, R. J., & Puchtel, I. S. (2010). Osmium isotope and highly siderophile element systematics of the Paraná Flood Basalt Province: implications for mantle sources. In Eos Transactions AGU, v.91, n.26, Meeting of the Americas Supplement, abstract V21B-02, 2010. Washington: American Geophysical Union.NLM
Rocha Júnior ERV, Marques LS, Walker RJ, Puchtel IS. Osmium isotope and highly siderophile element systematics of the Paraná Flood Basalt Province: implications for mantle sources. Eos Transactions AGU, v.91, n.26, Meeting of the Americas Supplement, abstract V21B-02, 2010. 2010 ;[citado 2024 out. 31 ]Vancouver
Rocha Júnior ERV, Marques LS, Walker RJ, Puchtel IS. Osmium isotope and highly siderophile element systematics of the Paraná Flood Basalt Province: implications for mantle sources. Eos Transactions AGU, v.91, n.26, Meeting of the Americas Supplement, abstract V21B-02, 2010. 2010 ;[citado 2024 out. 31 ]