Filtros : "OROGÊNESE" "Reino Unido" Removidos: "NEOPROTEROZOICO" "Asosiación Geologica Argentina" "GEOSUDESTE 2017" Limpar

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  • Source: International Geology Review. Unidades: IGC, IAG

    Subjects: OROGÊNESE, GEOCRONOLOGIA, METAMORFISMO

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    • ABNT

      FREITAS, Gabriela Bueno Fagundes de et al. Metamorphic and geochronological constraints on the final assembly of West Gondwana: an Ediacaran-Cambrian collisional setting in the northern Araguaia Orogen, central Brazil. International Geology Review, n. , p. 1-23-, 2023Tradução . . Disponível em: https://doi.org/10.1080/00206814.2023.2262695. Acesso em: 19 nov. 2024.
    • APA

      Freitas, G. B. F. de, Meira, V. T., Cioffi, C. R., Rocha, B. C. da, Luvizotto, G. L., Vervoort, J., & Trindade, R. I. F. da. (2023). Metamorphic and geochronological constraints on the final assembly of West Gondwana: an Ediacaran-Cambrian collisional setting in the northern Araguaia Orogen, central Brazil. International Geology Review, ( ), 1-23-. doi:10.1080/00206814.2023.2262695
    • NLM

      Freitas GBF de, Meira VT, Cioffi CR, Rocha BC da, Luvizotto GL, Vervoort J, Trindade RIF da. Metamorphic and geochronological constraints on the final assembly of West Gondwana: an Ediacaran-Cambrian collisional setting in the northern Araguaia Orogen, central Brazil [Internet]. International Geology Review. 2023 ;( ): 1-23-.[citado 2024 nov. 19 ] Available from: https://doi.org/10.1080/00206814.2023.2262695
    • Vancouver

      Freitas GBF de, Meira VT, Cioffi CR, Rocha BC da, Luvizotto GL, Vervoort J, Trindade RIF da. Metamorphic and geochronological constraints on the final assembly of West Gondwana: an Ediacaran-Cambrian collisional setting in the northern Araguaia Orogen, central Brazil [Internet]. International Geology Review. 2023 ;( ): 1-23-.[citado 2024 nov. 19 ] Available from: https://doi.org/10.1080/00206814.2023.2262695
  • Source: Journal of the Geological Society. Unidade: IGC

    Subjects: OROGÊNESE, GEOLOGIA ESTRUTURAL

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    • ABNT

      LARROVERE, Mariano Alexis et al. Mid-crustal deformation in a continental margin orogen: structural evolution and timing of the Famatinian Orogeny, NW Argentina. Journal of the Geological Society, v. 177, n. 2, p. 233-257, 2019Tradução . . Disponível em: https://doi.org/10.1144/jgs2018-230. Acesso em: 19 nov. 2024.
    • APA

      Larrovere, M. A., De los Hoyos, C. R., Willner, A. P., Verdecchia, S. O., Baldo, E. G., Casquet, C., et al. (2019). Mid-crustal deformation in a continental margin orogen: structural evolution and timing of the Famatinian Orogeny, NW Argentina. Journal of the Geological Society, 177( 2), 233-257. doi:10.1144/jgs2018-230
    • NLM

      Larrovere MA, De los Hoyos CR, Willner AP, Verdecchia SO, Baldo EG, Casquet C, Basei MAS, Hollanda MHBM de, Rocher S, Alasino P, Moreno GG. Mid-crustal deformation in a continental margin orogen: structural evolution and timing of the Famatinian Orogeny, NW Argentina [Internet]. Journal of the Geological Society. 2019 ; 177( 2): 233-257.[citado 2024 nov. 19 ] Available from: https://doi.org/10.1144/jgs2018-230
    • Vancouver

      Larrovere MA, De los Hoyos CR, Willner AP, Verdecchia SO, Baldo EG, Casquet C, Basei MAS, Hollanda MHBM de, Rocher S, Alasino P, Moreno GG. Mid-crustal deformation in a continental margin orogen: structural evolution and timing of the Famatinian Orogeny, NW Argentina [Internet]. Journal of the Geological Society. 2019 ; 177( 2): 233-257.[citado 2024 nov. 19 ] Available from: https://doi.org/10.1144/jgs2018-230
  • Source: Nature Communications. Unidade: IGC

    Subjects: TECTÔNICA DE PLACAS, OROGÊNESE, GONDWANA

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    • 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: 19 nov. 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 nov. 19 ] 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 nov. 19 ] Available from: https://doi.org/10.1038/ncomms6198
  • Source: Journal of the Geological Society. Unidade: IGC

    Subjects: ISÓTOPOS, OROGÊNESE, ÍNDIA

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    • ABNT

      BHATTACHARYA, S. et al. High-temperature crustal anatexis in a clockwise P-T-t path: isotopic evidence from a granulite-granitoid suite in the Eastern Ghats belt, India. Journal of the Geological Society, v. 160, n. 1, p. 39-46, 2003Tradução . . Disponível em: https://doi.org/10.1144/0016-764902-063. Acesso em: 19 nov. 2024.
    • APA

      Bhattacharya, S., Kar, R., Teixeira, W., & Basei, M. A. S. (2003). High-temperature crustal anatexis in a clockwise P-T-t path: isotopic evidence from a granulite-granitoid suite in the Eastern Ghats belt, India. Journal of the Geological Society, 160( 1), 39-46. doi:10.1144/0016-764902-063
    • NLM

      Bhattacharya S, Kar R, Teixeira W, Basei MAS. High-temperature crustal anatexis in a clockwise P-T-t path: isotopic evidence from a granulite-granitoid suite in the Eastern Ghats belt, India [Internet]. Journal of the Geological Society. 2003 ; 160( 1): 39-46.[citado 2024 nov. 19 ] Available from: https://doi.org/10.1144/0016-764902-063
    • Vancouver

      Bhattacharya S, Kar R, Teixeira W, Basei MAS. High-temperature crustal anatexis in a clockwise P-T-t path: isotopic evidence from a granulite-granitoid suite in the Eastern Ghats belt, India [Internet]. Journal of the Geological Society. 2003 ; 160( 1): 39-46.[citado 2024 nov. 19 ] Available from: https://doi.org/10.1144/0016-764902-063
  • Source: Journal of South American Earth Sciences. Unidade: IGC

    Assunto: OROGÊNESE

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    • ABNT

      CAMPOS NETO, Mario da Costa e FIGUEIREDO, Mário Cesar Heredia de. The Rio Doce orogeny, southeastern Brazil. Journal of South American Earth Sciences, v. 8, n. 2, p. 143-162, 1995Tradução . . Disponível em: https://doi.org/10.1016/0895-9811(95)00002-W. Acesso em: 19 nov. 2024.
    • APA

      Campos Neto, M. da C., & Figueiredo, M. C. H. de. (1995). The Rio Doce orogeny, southeastern Brazil. Journal of South American Earth Sciences, 8( 2), 143-162. doi:10.1016/0895-9811(95)00002-W
    • NLM

      Campos Neto M da C, Figueiredo MCH de. The Rio Doce orogeny, southeastern Brazil [Internet]. Journal of South American Earth Sciences. 1995 ; 8( 2): 143-162.[citado 2024 nov. 19 ] Available from: https://doi.org/10.1016/0895-9811(95)00002-W
    • Vancouver

      Campos Neto M da C, Figueiredo MCH de. The Rio Doce orogeny, southeastern Brazil [Internet]. Journal of South American Earth Sciences. 1995 ; 8( 2): 143-162.[citado 2024 nov. 19 ] Available from: https://doi.org/10.1016/0895-9811(95)00002-W

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