Filtros : "Financiamento DFG" "IGC-GMG" Removido: "2016" Limpar

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  • Source: Geochemistry. Unidade: IGC

    Subjects: BASALTO, PETROLOGIA

    PrivadoAcesso à fonteAcesso à fonteDOIHow to cite
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    • ABNT

      MACÊDO FILHO, Antomat Avelino et al. Petrology of Cenomanian basalts on the Brazilian equatorial margin: implications for the tectonomagmatic evolution of the drift phase. Geochemistry, v. 85, n. 1, p. 126248-, 2025Tradução . . Disponível em: https://doi.org/10.1016/j.chemer.2025.126248. Acesso em: 04 nov. 2025.
    • APA

      Macêdo Filho, A. A., Oliveira, A. L., Klöcking, M., Janasi, V. de A., Archanjo, C. J., & Lino, L. M. (2025). Petrology of Cenomanian basalts on the Brazilian equatorial margin: implications for the tectonomagmatic evolution of the drift phase. Geochemistry, 85( 1), 126248-. doi:10.1016/j.chemer.2025.126248
    • NLM

      Macêdo Filho AA, Oliveira AL, Klöcking M, Janasi V de A, Archanjo CJ, Lino LM. Petrology of Cenomanian basalts on the Brazilian equatorial margin: implications for the tectonomagmatic evolution of the drift phase [Internet]. Geochemistry. 2025 ; 85( 1): 126248-.[citado 2025 nov. 04 ] Available from: https://doi.org/10.1016/j.chemer.2025.126248
    • Vancouver

      Macêdo Filho AA, Oliveira AL, Klöcking M, Janasi V de A, Archanjo CJ, Lino LM. Petrology of Cenomanian basalts on the Brazilian equatorial margin: implications for the tectonomagmatic evolution of the drift phase [Internet]. Geochemistry. 2025 ; 85( 1): 126248-.[citado 2025 nov. 04 ] Available from: https://doi.org/10.1016/j.chemer.2025.126248
  • Source: International Journal of Earth Sciences. Unidade: IGC

    Subjects: ISÓTOPOS, OROGÊNESE, MAGMATISMO, PALEOGEOGRAFIA

    Versão PublicadaAcesso à fonteDOIHow to cite
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    • ABNT

      VESELÁ, P. et al. The detrital zircon record of Variscan to post‐Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps). International Journal of Earth Sciences, n. , p. , 2022Tradução . . Disponível em: https://doi.org/10.1007/s00531-022-02179-0. Acesso em: 04 nov. 2025.
    • APA

      Veselá, P., Oriolo, S., Basei, M. A. S., Lammerer, B., & Siegesmund, S. (2022). The detrital zircon record of Variscan to post‐Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps). International Journal of Earth Sciences, ( ), . doi:10.1007/s00531-022-02179-0
    • NLM

      Veselá P, Oriolo S, Basei MAS, Lammerer B, Siegesmund S. The detrital zircon record of Variscan to post‐Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps) [Internet]. International Journal of Earth Sciences. 2022 ;( ): .[citado 2025 nov. 04 ] Available from: https://doi.org/10.1007/s00531-022-02179-0
    • Vancouver

      Veselá P, Oriolo S, Basei MAS, Lammerer B, Siegesmund S. The detrital zircon record of Variscan to post‐Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps) [Internet]. International Journal of Earth Sciences. 2022 ;( ): .[citado 2025 nov. 04 ] Available from: https://doi.org/10.1007/s00531-022-02179-0
  • Source: Earth and Planetary Science Letters. Unidades: EACH, IAG, IGC

    Subjects: PALEOCEANOGRAFIA, SEDIMENTOLOGIA MARINHA

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    • ABNT

      ZHANG, Yancheng et al. Origin of increased terrigenous supply to the NE South American continental margin during Heinrich Stadial 1 and the Younger Dryas. Earth and Planetary Science Letters, v. 432, p. 493-500, 2015Tradução . . Disponível em: https://doi.org/10.1016/j.epsl.2015.09.054. Acesso em: 04 nov. 2025.
    • APA

      Zhang, Y., Chiessi, C. M., Mulitza, S., Zabel, M., Trindade, R. I. F. da, Hollanda, M. H. B. M. de, et al. (2015). Origin of increased terrigenous supply to the NE South American continental margin during Heinrich Stadial 1 and the Younger Dryas. Earth and Planetary Science Letters, 432, 493-500. doi:10.1016/j.epsl.2015.09.054
    • NLM

      Zhang Y, Chiessi CM, Mulitza S, Zabel M, Trindade RIF da, Hollanda MHBM de, Dantas EL, Govin A, Tiedemann R, Wefer G. Origin of increased terrigenous supply to the NE South American continental margin during Heinrich Stadial 1 and the Younger Dryas [Internet]. Earth and Planetary Science Letters. 2015 ; 432 493-500.[citado 2025 nov. 04 ] Available from: https://doi.org/10.1016/j.epsl.2015.09.054
    • Vancouver

      Zhang Y, Chiessi CM, Mulitza S, Zabel M, Trindade RIF da, Hollanda MHBM de, Dantas EL, Govin A, Tiedemann R, Wefer G. Origin of increased terrigenous supply to the NE South American continental margin during Heinrich Stadial 1 and the Younger Dryas [Internet]. Earth and Planetary Science Letters. 2015 ; 432 493-500.[citado 2025 nov. 04 ] Available from: https://doi.org/10.1016/j.epsl.2015.09.054

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