Sato, Kei 
; Siga Júnior, Oswaldo ; Silva, Josiane Aline da; McReath, Ian; Liu, Dunyi ; Tsuyoshi, Lizuka; Rino, Shuji; Hirata, Takafumi; Sproesser, Walter Maurício; Basei, Miguel Angelo Stipp
Source: Geologia USP. Série Científica. Unidade: IGC
Subjects: ZIRCÃO, COMPOSIÇÃO ISOTÓPICA
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SATO, Kei et al. In situ isotopic analyses of U and Pb in zircon by remotely operated SHRIMP II, and Hf by LA-ICP-MS: an example of dating and genetic evolution of zircon by 176Hf/177Hf from the Ita Quarry in the Atuba Complex, SE Brazil. Geologia USP. Série Científica, v. 9, n. 3, p. 61-69, 2009Tradução . . Disponível em: https://doi.org/10.5327/z1519-874x2009000300004. Acesso em: 19 nov. 2024.APA
Sato, K., Siga Júnior, O., Silva, J. A. da, McReath, I., Liu, D., Tsuyoshi, L., et al. (2009). In situ isotopic analyses of U and Pb in zircon by remotely operated SHRIMP II, and Hf by LA-ICP-MS: an example of dating and genetic evolution of zircon by 176Hf/177Hf from the Ita Quarry in the Atuba Complex, SE Brazil. Geologia USP. Série Científica, 9( 3), 61-69. doi:10.5327/z1519-874x2009000300004NLM
Sato K, Siga Júnior O, Silva JA da, McReath I, Liu D, Tsuyoshi L, Rino S, Hirata T, Sproesser WM, Basei MAS. In situ isotopic analyses of U and Pb in zircon by remotely operated SHRIMP II, and Hf by LA-ICP-MS: an example of dating and genetic evolution of zircon by 176Hf/177Hf from the Ita Quarry in the Atuba Complex, SE Brazil [Internet]. Geologia USP. Série Científica. 2009 ; 9( 3): 61-69.[citado 2024 nov. 19 ] Available from: https://doi.org/10.5327/z1519-874x2009000300004Vancouver
Sato K, Siga Júnior O, Silva JA da, McReath I, Liu D, Tsuyoshi L, Rino S, Hirata T, Sproesser WM, Basei MAS. In situ isotopic analyses of U and Pb in zircon by remotely operated SHRIMP II, and Hf by LA-ICP-MS: an example of dating and genetic evolution of zircon by 176Hf/177Hf from the Ita Quarry in the Atuba Complex, SE Brazil [Internet]. Geologia USP. Série Científica. 2009 ; 9( 3): 61-69.[citado 2024 nov. 19 ] Available from: https://doi.org/10.5327/z1519-874x2009000300004
