4.4 billion years of crustal maturation: oxygen isotope ratios of magmatic zircon (2005)
Fonte: Contributions to Mineralogy and Petrology. Unidade: IGC
Assuntos: CROSTA DA TERRA, ZIRCÃO, GEOQUÍMICA ISOTÓPICA, GEOCRONOLOGIA
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VALLEY, J. W. et al. 4.4 billion years of crustal maturation: oxygen isotope ratios of magmatic zircon. Contributions to Mineralogy and Petrology, v. 150, n. 6, p. 561-580, 2005Tradução . . Disponível em: https://doi.org/10.1007/s00410-005-0025-8. Acesso em: 01 nov. 2024.APA
Valley, J. W., Lackey, J. S., Cavosie, A. J., Clechenko, C. C., Spicuzza, M. J., Basei, M. A. S., et al. (2005). 4.4 billion years of crustal maturation: oxygen isotope ratios of magmatic zircon. Contributions to Mineralogy and Petrology, 150( 6), 561-580. doi:10.1007/s00410-005-0025-8NLM
Valley JW, Lackey JS, Cavosie AJ, Clechenko CC, Spicuzza MJ, Basei MAS, Bindeman IN, Ferreira V, Sial AN, King EM, Peck WH, Sinha AK, Wei CS. 4.4 billion years of crustal maturation: oxygen isotope ratios of magmatic zircon [Internet]. Contributions to Mineralogy and Petrology. 2005 ;150( 6): 561-580.[citado 2024 nov. 01 ] Available from: https://doi.org/10.1007/s00410-005-0025-8Vancouver
Valley JW, Lackey JS, Cavosie AJ, Clechenko CC, Spicuzza MJ, Basei MAS, Bindeman IN, Ferreira V, Sial AN, King EM, Peck WH, Sinha AK, Wei CS. 4.4 billion years of crustal maturation: oxygen isotope ratios of magmatic zircon [Internet]. Contributions to Mineralogy and Petrology. 2005 ;150( 6): 561-580.[citado 2024 nov. 01 ] Available from: https://doi.org/10.1007/s00410-005-0025-8