Provenance of the Ediacaran Salinas Formation (Araçuaí Orogen, Brazil): Clues from lithochemical data and zircon U-Pb (SHRIMP) ages of volcanic clasts (2019)
- Authors:
- USP affiliated authors: CORDANI, UMBERTO GIUSEPPE - IGC ; SATO, KEI - IGC
- Unidade: IGC
- DOI: 10.1590/2317-4889201920190017
- Subjects: PETROLOGIA; EVOLUÇÃO TECTÔNICA; GEOQUÍMICA
- Language: Inglês
- Source:
- Título: Brazilian Journal of Geology
- ISSN: 2317-4692
- Volume/Número/Paginação/Ano: v. 49, n. 2, p., 2019
- Status:
- Artigo publicado em periódico de acesso aberto (Gold Open Access)
- Versão do Documento:
- Versão publicada (Published version)
- Acessar versão aberta:
-
ABNT
DELUCA, Carolina et al. Provenance of the Ediacaran Salinas Formation (Araçuaí Orogen, Brazil): Clues from lithochemical data and zircon U-Pb (SHRIMP) ages of volcanic clasts. Brazilian Journal of Geology, v. 49, n. 2, p. , 2019Tradução . . Disponível em: https://doi.org/10.1590/2317-4889201920190017. Acesso em: 07 maio 2026. -
APA
Deluca, C., Pedrosa-Soares, A. C., Lima, S., Cordani, U. G., & Sato, K. (2019). Provenance of the Ediacaran Salinas Formation (Araçuaí Orogen, Brazil): Clues from lithochemical data and zircon U-Pb (SHRIMP) ages of volcanic clasts. Brazilian Journal of Geology, 49( 2), . doi:10.1590/2317-4889201920190017 -
NLM
Deluca C, Pedrosa-Soares AC, Lima S, Cordani UG, Sato K. Provenance of the Ediacaran Salinas Formation (Araçuaí Orogen, Brazil): Clues from lithochemical data and zircon U-Pb (SHRIMP) ages of volcanic clasts [Internet]. Brazilian Journal of Geology. 2019 ; 49( 2): .[citado 2026 maio 07 ] Available from: https://doi.org/10.1590/2317-4889201920190017 -
Vancouver
Deluca C, Pedrosa-Soares AC, Lima S, Cordani UG, Sato K. Provenance of the Ediacaran Salinas Formation (Araçuaí Orogen, Brazil): Clues from lithochemical data and zircon U-Pb (SHRIMP) ages of volcanic clasts [Internet]. Brazilian Journal of Geology. 2019 ; 49( 2): .[citado 2026 maio 07 ] Available from: https://doi.org/10.1590/2317-4889201920190017 - Geochronological systematics of the Huayna Potosi and Zongo granitic plutons, Cordillera Real of Bolivia, by the K/Ar, Rb/Sr and U/Pb methods
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