Filtros : "D'Agrella Filho, Manoel Souza" "Reino Unido" Removido: "Anais: Boletim de resumos" Limpar

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  • Source: Large Igneous Provinces and their Plumbing Systems. Unidades: IGC, IAG

    Subjects: ROCHAS MAGMÁTICAS, METALOGÊNESE

    PrivadoAcesso à fonteDOIHow to cite
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    • ABNT

      REIS, Nelson Joaquim et al. Large igneous provinces of the Amazonian Craton and their metallogenic potential in Proterozoic times. Large Igneous Provinces and their Plumbing Systems, n. 518, p. 493-529-, 2021Tradução . . Disponível em: https://doi.org/10.1144/SP518-2021-7. Acesso em: 16 out. 2024.
    • APA

      Reis, N. J., Teixeira, W., D'Agrella Filho, M. S., Bettencourt, J. S., Ernst, R. E., & Goulart, L. E. A. (2021). Large igneous provinces of the Amazonian Craton and their metallogenic potential in Proterozoic times. Large Igneous Provinces and their Plumbing Systems, ( 518), 493-529-. doi:10.1144/SP518-2021-7
    • NLM

      Reis NJ, Teixeira W, D'Agrella Filho MS, Bettencourt JS, Ernst RE, Goulart LEA. Large igneous provinces of the Amazonian Craton and their metallogenic potential in Proterozoic times [Internet]. Large Igneous Provinces and their Plumbing Systems. 2021 ;( 518): 493-529-.[citado 2024 out. 16 ] Available from: https://doi.org/10.1144/SP518-2021-7
    • Vancouver

      Reis NJ, Teixeira W, D'Agrella Filho MS, Bettencourt JS, Ernst RE, Goulart LEA. Large igneous provinces of the Amazonian Craton and their metallogenic potential in Proterozoic times [Internet]. Large Igneous Provinces and their Plumbing Systems. 2021 ;( 518): 493-529-.[citado 2024 out. 16 ] Available from: https://doi.org/10.1144/SP518-2021-7
  • Source: Journal of South American Earth Sciences. Unidade: IAG

    Subjects: DIQUES, MAGMATISMO, MAGMA, TUCUMÃ (PA)

    Acesso à fonteDOIHow to cite
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    • ABNT

      SILVA, Fernando Fernandes da et al. Bimodal magmatism of the Tucumã area, Carajás province: U-Pb geochronology, classification and processes. Journal of South American Earth Sciences, v. 72, p. 95-114, 2016Tradução . . Disponível em: https://doi.org/10.1016/j.jsames.2016.07.016. Acesso em: 16 out. 2024.
    • APA

      Silva, F. F. da, Oliveira, D. C. de, Antonio, P. Y. J., D'Agrella Filho, M. S., & Lamarão, C. N. (2016). Bimodal magmatism of the Tucumã area, Carajás province: U-Pb geochronology, classification and processes. Journal of South American Earth Sciences, 72, 95-114. doi:10.1016/j.jsames.2016.07.016
    • NLM

      Silva FF da, Oliveira DC de, Antonio PYJ, D'Agrella Filho MS, Lamarão CN. Bimodal magmatism of the Tucumã area, Carajás province: U-Pb geochronology, classification and processes [Internet]. Journal of South American Earth Sciences. 2016 ;72 95-114.[citado 2024 out. 16 ] Available from: https://doi.org/10.1016/j.jsames.2016.07.016
    • Vancouver

      Silva FF da, Oliveira DC de, Antonio PYJ, D'Agrella Filho MS, Lamarão CN. Bimodal magmatism of the Tucumã area, Carajás province: U-Pb geochronology, classification and processes [Internet]. Journal of South American Earth Sciences. 2016 ;72 95-114.[citado 2024 out. 16 ] Available from: https://doi.org/10.1016/j.jsames.2016.07.016
  • Source: Geological Society Special Publications. Unidade: IAG

    Subjects: PALEOMAGNETISMO, CRÁTON, ENXAME DE DIQUES

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    • ABNT

      EVANS, D. A. D et al. Return to Rodinia?: Moderate to high palaeolatitude of the São Francisco/Congo craton at 920 Ma. Geological Society Special Publications, v. 424, p. 1-24, 2015Tradução . . Disponível em: https://doi.org/10.1144/SP424.1. Acesso em: 16 out. 2024.
    • APA

      Evans, D. A. D., Trindade, R. I. F. da, Catelani, E. L., D'Agrella Filho, M. S., Heaman, L. M., Oliveira, E. P., et al. (2015). Return to Rodinia?: Moderate to high palaeolatitude of the São Francisco/Congo craton at 920 Ma. Geological Society Special Publications, 424, 1-24. doi:10.1144/SP424.1
    • NLM

      Evans DAD, Trindade RIF da, Catelani EL, D'Agrella Filho MS, Heaman LM, Oliveira EP, Söderlund U, Ernst RE, Smirnov AV, Salminen JM. Return to Rodinia?: Moderate to high palaeolatitude of the São Francisco/Congo craton at 920 Ma [Internet]. Geological Society Special Publications. 2015 ; 424 1-24.[citado 2024 out. 16 ] Available from: https://doi.org/10.1144/SP424.1
    • Vancouver

      Evans DAD, Trindade RIF da, Catelani EL, D'Agrella Filho MS, Heaman LM, Oliveira EP, Söderlund U, Ernst RE, Smirnov AV, Salminen JM. Return to Rodinia?: Moderate to high palaeolatitude of the São Francisco/Congo craton at 920 Ma [Internet]. Geological Society Special Publications. 2015 ; 424 1-24.[citado 2024 out. 16 ] Available from: https://doi.org/10.1144/SP424.1
  • Source: Journal of South American Earth Sciences. Unidade: IAG

    Subjects: GEOFÍSICA, PALEOMAGNETISMO

    Acesso à fonteDOIHow to cite
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    • ABNT

      D'AGRELLA FILHO, Manoel Souza e PACCA, Igor Ivory Gil. Paleomagnetism of Paleoproterozoic mafic dyke swarm from the Uauá region, northeastern São Francisco Craton, Brazil: tectonic implications. Journal of South American Earth Sciences, v. 11, n. 1, p. 23-33, 1998Tradução . . Disponível em: https://doi.org/10.1016/s0895-9811(97)00034-5. Acesso em: 16 out. 2024.
    • APA

      D'Agrella Filho, M. S., & Pacca, I. I. G. (1998). Paleomagnetism of Paleoproterozoic mafic dyke swarm from the Uauá region, northeastern São Francisco Craton, Brazil: tectonic implications. Journal of South American Earth Sciences, 11( 1), 23-33. doi:10.1016/s0895-9811(97)00034-5
    • NLM

      D'Agrella Filho MS, Pacca IIG. Paleomagnetism of Paleoproterozoic mafic dyke swarm from the Uauá region, northeastern São Francisco Craton, Brazil: tectonic implications [Internet]. Journal of South American Earth Sciences. 1998 ; 11( 1): 23-33.[citado 2024 out. 16 ] Available from: https://doi.org/10.1016/s0895-9811(97)00034-5
    • Vancouver

      D'Agrella Filho MS, Pacca IIG. Paleomagnetism of Paleoproterozoic mafic dyke swarm from the Uauá region, northeastern São Francisco Craton, Brazil: tectonic implications [Internet]. Journal of South American Earth Sciences. 1998 ; 11( 1): 23-33.[citado 2024 out. 16 ] Available from: https://doi.org/10.1016/s0895-9811(97)00034-5

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