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Filtros : "Hermann, Joerg" Limpar

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  • Artigo de periodico

    Magmatic flare-up causes crustal thickening at the transition from subduction to continental collision (2021)

    Ganade, Carlos E. ; Lanari, Pierre ; Rubatto, Daniela ; Hermann, Joerg ; Weinberg, Roberto F. ; Basei, Miguel Angelo Stipp ; Tesser, Lucas R. ; Caby, Renaud; Agbossoumounde, Yao; Ribeiro, Caroline M.

    Source: Communications Earth & Environment. Unidade: IGC

    Subjects: GEOCRONOLOGIA, MAGMA, MAGMATISMO

    Versão PublicadaAcesso à fonteDOIHow to cite
    A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas

    • ABNT

      GANADE, Carlos E. et al. Magmatic flare-up causes crustal thickening at the transition from subduction to continental collision. Communications Earth & Environment, v. 2, n. 41, p. -, 2021Tradução . . Disponível em: https://doi.org/10.1038/s43247-021-00103-z. Acesso em: 12 maio 2024.

    • APA

      Ganade, C. E., Lanari, P., Rubatto, D., Hermann, J., Weinberg, R. F., Basei, M. A. S., et al. (2021). Magmatic flare-up causes crustal thickening at the transition from subduction to continental collision. Communications Earth & Environment, 2( 41), -. doi:10.1038/s43247-021-00103-z

    • NLM

      Ganade CE, Lanari P, Rubatto D, Hermann J, Weinberg RF, Basei MAS, Tesser LR, Caby R, Agbossoumounde Y, Ribeiro CM. Magmatic flare-up causes crustal thickening at the transition from subduction to continental collision [Internet]. Communications Earth & Environment. 2021 ; 2( 41): -.[citado 2024 maio 12 ] Available from: https://doi.org/10.1038/s43247-021-00103-z

    • Vancouver

      Ganade CE, Lanari P, Rubatto D, Hermann J, Weinberg RF, Basei MAS, Tesser LR, Caby R, Agbossoumounde Y, Ribeiro CM. Magmatic flare-up causes crustal thickening at the transition from subduction to continental collision [Internet]. Communications Earth & Environment. 2021 ; 2( 41): -.[citado 2024 maio 12 ] Available from: https://doi.org/10.1038/s43247-021-00103-z

  • Artigo de periodico

    Ediacaran 2,500-km-long synchronous deep continental subduction in the West Gondwana Orogen (2014)

    Ganade, Carlos E. ; Rubatto, Daniela ; Hermann, Joerg ; Cordani, Umberto G. ; Caby, Renaud; Basei, Miguel Angelo Stipp

    Source: Nature Communications. Unidade: IGC

    Subjects: TECTÔNICA DE PLACAS, OROGÊNESE, GONDWANA

    Versão PublicadaAcesso à fonteDOIHow to cite
    A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas

    • ABNT

      GANADE, Carlos E. et al. Ediacaran 2,500-km-long synchronous deep continental subduction in the West Gondwana Orogen. Nature Communications, v. 5, n. 5198, p. 1-8, 2014Tradução . . Disponível em: https://doi.org/10.1038/ncomms6198. Acesso em: 12 maio 2024.

    • APA

      Ganade, C. E., Rubatto, D., Hermann, J., Cordani, U. G., Caby, R., & Basei, M. A. S. (2014). Ediacaran 2,500-km-long synchronous deep continental subduction in the West Gondwana Orogen. Nature Communications, 5( 5198), 1-8. doi:10.1038/ncomms6198

    • NLM

      Ganade CE, Rubatto D, Hermann J, Cordani UG, Caby R, Basei MAS. Ediacaran 2,500-km-long synchronous deep continental subduction in the West Gondwana Orogen [Internet]. Nature Communications. 2014 ; 5( 5198): 1-8.[citado 2024 maio 12 ] Available from: https://doi.org/10.1038/ncomms6198

    • Vancouver

      Ganade CE, Rubatto D, Hermann J, Cordani UG, Caby R, Basei MAS. Ediacaran 2,500-km-long synchronous deep continental subduction in the West Gondwana Orogen [Internet]. Nature Communications. 2014 ; 5( 5198): 1-8.[citado 2024 maio 12 ] Available from: https://doi.org/10.1038/ncomms6198
  • 1

1 - 2 (2 records)

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