Filtros : "Tassinari, Colombo Celso Gaeta" "Financiado pela FCT" Removido: "TRABALHO DE EVENTO" Limpar

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  • Source: Marine and Petroleum Geology. Unidade: IGC

    Subjects: JURÁSSICO, GEOQUÍMICA INORGÂNICA, ROCHAS SEDIMENTARES, PETRÓLEO

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    • ABNT

      FERREIRA, Ezequiel et al. Tracing bottom-water redox conditions during deposition of Lower and Upper Jurassic organic-rich sedimentary rocks in the Lusitanian Basin (Portugal): insights from inorganic geochemistry. Marine and Petroleum Geology, v. 117, n. , p. 104343, 2020Tradução . . Disponível em: https://doi.org/10.1016/j.marpetgeo.2020.104343. Acesso em: 14 jun. 2024.
    • APA

      Ferreira, E., Mateus, A., Azerêdo, A. C., Duarte, L. V., Mendonça-Filho, J., & Tassinari, C. C. G. (2020). Tracing bottom-water redox conditions during deposition of Lower and Upper Jurassic organic-rich sedimentary rocks in the Lusitanian Basin (Portugal): insights from inorganic geochemistry. Marine and Petroleum Geology, 117( ), 104343. doi:10.1016/j.marpetgeo.2020.104343
    • NLM

      Ferreira E, Mateus A, Azerêdo AC, Duarte LV, Mendonça-Filho J, Tassinari CCG. Tracing bottom-water redox conditions during deposition of Lower and Upper Jurassic organic-rich sedimentary rocks in the Lusitanian Basin (Portugal): insights from inorganic geochemistry [Internet]. Marine and Petroleum Geology. 2020 ; 117( ): 104343.[citado 2024 jun. 14 ] Available from: https://doi.org/10.1016/j.marpetgeo.2020.104343
    • Vancouver

      Ferreira E, Mateus A, Azerêdo AC, Duarte LV, Mendonça-Filho J, Tassinari CCG. Tracing bottom-water redox conditions during deposition of Lower and Upper Jurassic organic-rich sedimentary rocks in the Lusitanian Basin (Portugal): insights from inorganic geochemistry [Internet]. Marine and Petroleum Geology. 2020 ; 117( ): 104343.[citado 2024 jun. 14 ] Available from: https://doi.org/10.1016/j.marpetgeo.2020.104343
  • Source: Ore Geology Reviews. Unidade: IGC

    Subjects: GEOQUÍMICA, PESQUISA MINERAL

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    • ABNT

      LUZ, Filipa et al. Recognizing metasedimentary sequences potentially hosting concealed massive sulfide accumulations in the Iberian Pyrite Belt using geochemical fingerprints. Ore Geology Reviews, v. 107, n. , p. 973-998, 2019Tradução . . Disponível em: https://doi.org/10.1016/j.oregeorev.2019.03.020. Acesso em: 14 jun. 2024.
    • APA

      Luz, F., Mateus, A., Figueira, J., Tassinari, C. C. G., Ferreira, E., & Gonçalves, L. (2019). Recognizing metasedimentary sequences potentially hosting concealed massive sulfide accumulations in the Iberian Pyrite Belt using geochemical fingerprints. Ore Geology Reviews, 107( ), 973-998. doi:10.1016/j.oregeorev.2019.03.020
    • NLM

      Luz F, Mateus A, Figueira J, Tassinari CCG, Ferreira E, Gonçalves L. Recognizing metasedimentary sequences potentially hosting concealed massive sulfide accumulations in the Iberian Pyrite Belt using geochemical fingerprints [Internet]. Ore Geology Reviews. 2019 ; 107( ): 973-998.[citado 2024 jun. 14 ] Available from: https://doi.org/10.1016/j.oregeorev.2019.03.020
    • Vancouver

      Luz F, Mateus A, Figueira J, Tassinari CCG, Ferreira E, Gonçalves L. Recognizing metasedimentary sequences potentially hosting concealed massive sulfide accumulations in the Iberian Pyrite Belt using geochemical fingerprints [Internet]. Ore Geology Reviews. 2019 ; 107( ): 973-998.[citado 2024 jun. 14 ] Available from: https://doi.org/10.1016/j.oregeorev.2019.03.020
  • Source: Sedimentary Geology. Unidade: IGC

    Subjects: GEOCRONOLOGIA, PANGÉA, PALEOGEOGRAFIA

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    • ABNT

      DINIS, Pedro A. et al. The transition from Pangea amalgamation to fragmentation: constraints from detrital zircon geochronology on West Iberia paleogeography and sediment sources. Sedimentary Geology, v. 375, p. 172-187, 2018Tradução . . Disponível em: https://doi.org/10.1016/j.sedgeo.2017.09.015. Acesso em: 14 jun. 2024.
    • APA

      Dinis, P. A., Fernandes, P., Jorge, R. C. G. S., Rodrigues, B., Chew, D. M., & Tassinari, C. C. G. (2018). The transition from Pangea amalgamation to fragmentation: constraints from detrital zircon geochronology on West Iberia paleogeography and sediment sources. Sedimentary Geology, 375, 172-187. doi:10.1016/j.sedgeo.2017.09.015
    • NLM

      Dinis PA, Fernandes P, Jorge RCGS, Rodrigues B, Chew DM, Tassinari CCG. The transition from Pangea amalgamation to fragmentation: constraints from detrital zircon geochronology on West Iberia paleogeography and sediment sources [Internet]. Sedimentary Geology. 2018 ; 375 172-187.[citado 2024 jun. 14 ] Available from: https://doi.org/10.1016/j.sedgeo.2017.09.015
    • Vancouver

      Dinis PA, Fernandes P, Jorge RCGS, Rodrigues B, Chew DM, Tassinari CCG. The transition from Pangea amalgamation to fragmentation: constraints from detrital zircon geochronology on West Iberia paleogeography and sediment sources [Internet]. Sedimentary Geology. 2018 ; 375 172-187.[citado 2024 jun. 14 ] Available from: https://doi.org/10.1016/j.sedgeo.2017.09.015
  • Source: Tectonophysics. Unidade: IGC

    Subjects: ZIRCÃO, GEOCRONOLOGIA, GEODINÂMICA

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    • ABNT

      MATEUS, A. et al. U–Pb SHRIMP zircon dating of high-grade rocks from the Upper Allochthonous Terrane of Bragança and Morais Massifs (NE Portugal): geodynamic consequences. Tectonophysics, v. 675, p. 23-49, 2016Tradução . . Disponível em: https://doi.org/10.1016/j.tecto.2016.02.048. Acesso em: 14 jun. 2024.
    • APA

      Mateus, A., Munhá, J., Ribeiro, A., Tassinari, C. C. G., Sato, K., Pereira, E., & Santos, J. F. (2016). U–Pb SHRIMP zircon dating of high-grade rocks from the Upper Allochthonous Terrane of Bragança and Morais Massifs (NE Portugal): geodynamic consequences. Tectonophysics, 675, 23-49. doi:10.1016/j.tecto.2016.02.048
    • NLM

      Mateus A, Munhá J, Ribeiro A, Tassinari CCG, Sato K, Pereira E, Santos JF. U–Pb SHRIMP zircon dating of high-grade rocks from the Upper Allochthonous Terrane of Bragança and Morais Massifs (NE Portugal): geodynamic consequences [Internet]. Tectonophysics. 2016 ; 675 23-49.[citado 2024 jun. 14 ] Available from: https://doi.org/10.1016/j.tecto.2016.02.048
    • Vancouver

      Mateus A, Munhá J, Ribeiro A, Tassinari CCG, Sato K, Pereira E, Santos JF. U–Pb SHRIMP zircon dating of high-grade rocks from the Upper Allochthonous Terrane of Bragança and Morais Massifs (NE Portugal): geodynamic consequences [Internet]. Tectonophysics. 2016 ; 675 23-49.[citado 2024 jun. 14 ] Available from: https://doi.org/10.1016/j.tecto.2016.02.048

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