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  • Source: Tectonics. Unidade: IGC

    Subjects: EVOLUÇÃO TECTÔNICA, PALEOGEOGRAFIA, GONDWANA

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    • ABNT

      MEIRA, Vinícius Tieppo et al. Reply to Comment by Heilbron and Valeriano on “Tectono Metamorphic Evolution of the Central Ribeira Belt, Brazil:: a Case of Late Neoproterozoic Intracontinental Orogeny and Flow of Partially Molten Deep Crust During the Assembly of West Gondwana". Tectonics, v. 39, 2020Tradução . . Disponível em: https://doi.org/10.1029/2020TC006307. Acesso em: 29 jun. 2024.
    • APA

      Meira, V. T., Garcia-Casco, A., Hyppolito, T. N., Juliani, C., & Schorscher, J. H. D. (2020). Reply to Comment by Heilbron and Valeriano on “Tectono Metamorphic Evolution of the Central Ribeira Belt, Brazil:: a Case of Late Neoproterozoic Intracontinental Orogeny and Flow of Partially Molten Deep Crust During the Assembly of West Gondwana". Tectonics, 39. doi:10.1029/2020TC006307
    • NLM

      Meira VT, Garcia-Casco A, Hyppolito TN, Juliani C, Schorscher JHD. Reply to Comment by Heilbron and Valeriano on “Tectono Metamorphic Evolution of the Central Ribeira Belt, Brazil:: a Case of Late Neoproterozoic Intracontinental Orogeny and Flow of Partially Molten Deep Crust During the Assembly of West Gondwana" [Internet]. Tectonics. 2020 ; 39[citado 2024 jun. 29 ] Available from: https://doi.org/10.1029/2020TC006307
    • Vancouver

      Meira VT, Garcia-Casco A, Hyppolito TN, Juliani C, Schorscher JHD. Reply to Comment by Heilbron and Valeriano on “Tectono Metamorphic Evolution of the Central Ribeira Belt, Brazil:: a Case of Late Neoproterozoic Intracontinental Orogeny and Flow of Partially Molten Deep Crust During the Assembly of West Gondwana" [Internet]. Tectonics. 2020 ; 39[citado 2024 jun. 29 ] Available from: https://doi.org/10.1029/2020TC006307
  • Source: Tectonics. Unidade: IGC

    Subjects: EVOLUÇÃO TECTÔNICA, OROGÊNESE, GONDWANA

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    • ABNT

      MEIRA, Vinícius Tieppo et al. Tectono‐metamorphic evolution of the Central Ribeira Belt, Brazil: a case of late Neoproterozoic intracontinental orogeny and flow of partially molten deep crust during the assembly of West Gondwana. Tectonics, v. 38, n. 8, p. 3182-3209, 2019Tradução . . Disponível em: https://doi.org/10.1029/2018tc004959. Acesso em: 29 jun. 2024.
    • APA

      Meira, V. T., Garcia‐Casco, A., Hyppolito, T. N., Juliani, C., & Schorscher, J. H. D. (2019). Tectono‐metamorphic evolution of the Central Ribeira Belt, Brazil: a case of late Neoproterozoic intracontinental orogeny and flow of partially molten deep crust during the assembly of West Gondwana. Tectonics, 38( 8), 3182-3209. doi:10.1029/2018tc004959
    • NLM

      Meira VT, Garcia‐Casco A, Hyppolito TN, Juliani C, Schorscher JHD. Tectono‐metamorphic evolution of the Central Ribeira Belt, Brazil: a case of late Neoproterozoic intracontinental orogeny and flow of partially molten deep crust during the assembly of West Gondwana [Internet]. Tectonics. 2019 ; 38( 8): 3182-3209.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1029/2018tc004959
    • Vancouver

      Meira VT, Garcia‐Casco A, Hyppolito TN, Juliani C, Schorscher JHD. Tectono‐metamorphic evolution of the Central Ribeira Belt, Brazil: a case of late Neoproterozoic intracontinental orogeny and flow of partially molten deep crust during the assembly of West Gondwana [Internet]. Tectonics. 2019 ; 38( 8): 3182-3209.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1029/2018tc004959
  • Source: Precambrian Research. Unidade: IGC

    Subjects: EVOLUÇÃO TECTÔNICA, MAGMATISMO

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      MEIRA, Vinícius Tieppo et al. Late Tonian within-plate mafic magmatism and Ediacaran partial melting and magmatism in the Costeiro Domain, Central Ribeira Belt, Brazil. Precambrian Research, v. 334, n. , p. 105440, 2019Tradução . . Disponível em: https://doi.org/10.1016/j.precamres.2019.105440. Acesso em: 29 jun. 2024.
    • APA

      Meira, V. T., Garcia-Casco, A., Juliani, C., & Schorscher, J. H. D. (2019). Late Tonian within-plate mafic magmatism and Ediacaran partial melting and magmatism in the Costeiro Domain, Central Ribeira Belt, Brazil. Precambrian Research, 334( ), 105440. doi:10.1016/j.precamres.2019.105440
    • NLM

      Meira VT, Garcia-Casco A, Juliani C, Schorscher JHD. Late Tonian within-plate mafic magmatism and Ediacaran partial melting and magmatism in the Costeiro Domain, Central Ribeira Belt, Brazil [Internet]. Precambrian Research. 2019 ; 334( ): 105440.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1016/j.precamres.2019.105440
    • Vancouver

      Meira VT, Garcia-Casco A, Juliani C, Schorscher JHD. Late Tonian within-plate mafic magmatism and Ediacaran partial melting and magmatism in the Costeiro Domain, Central Ribeira Belt, Brazil [Internet]. Precambrian Research. 2019 ; 334( ): 105440.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1016/j.precamres.2019.105440
  • Source: GSA Bulletin. Unidade: IGC

    Subjects: EVOLUÇÃO TECTÔNICA, GEOCRONOLOGIA

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    • ABNT

      ANGIBOUST, Samuel et al. A 100-m.y.-long window onto mass-flow processes in the Patagonian Mesozoic subduction zone (Diego de Almagro Island, Chile). GSA Bulletin, v. 130, n. 9-10, p. 1439-1456, 2018Tradução . . Disponível em: https://doi.org/10.1130/b31891.1. Acesso em: 29 jun. 2024.
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      Angiboust, S., Cambeses, A., Hyppolito, T. N., Glodny, J., Monié, P., Calderón, M., & Juliani, C. (2018). A 100-m.y.-long window onto mass-flow processes in the Patagonian Mesozoic subduction zone (Diego de Almagro Island, Chile). GSA Bulletin, 130( 9-10), 1439-1456. doi:10.1130/b31891.1
    • NLM

      Angiboust S, Cambeses A, Hyppolito TN, Glodny J, Monié P, Calderón M, Juliani C. A 100-m.y.-long window onto mass-flow processes in the Patagonian Mesozoic subduction zone (Diego de Almagro Island, Chile) [Internet]. GSA Bulletin. 2018 ; 130( 9-10): 1439-1456.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1130/b31891.1
    • Vancouver

      Angiboust S, Cambeses A, Hyppolito TN, Glodny J, Monié P, Calderón M, Juliani C. A 100-m.y.-long window onto mass-flow processes in the Patagonian Mesozoic subduction zone (Diego de Almagro Island, Chile) [Internet]. GSA Bulletin. 2018 ; 130( 9-10): 1439-1456.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1130/b31891.1
  • Source: Geological Society, London, Special Publications. Unidade: IGC

    Subjects: PETROLOGIA METAMÓRFICA, OLIGOELEMENTOS

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    • ABNT

      HYPPOLITO, Thais Nogueira et al. Rehydration of eclogites and garnet-replacement processes during exhumation in the amphibolite facies. Geological Society, London, Special Publications, v. 478, n. 1, p. 217-239, 2018Tradução . . Disponível em: https://doi.org/10.1144/sp478.3. Acesso em: 29 jun. 2024.
    • APA

      Hyppolito, T. N., Cambeses, A., Angiboust, S., Raimondo, T., García-Casco, A., & Juliani, C. (2018). Rehydration of eclogites and garnet-replacement processes during exhumation in the amphibolite facies. Geological Society, London, Special Publications, 478( 1), 217-239. doi:10.1144/sp478.3
    • NLM

      Hyppolito TN, Cambeses A, Angiboust S, Raimondo T, García-Casco A, Juliani C. Rehydration of eclogites and garnet-replacement processes during exhumation in the amphibolite facies [Internet]. Geological Society, London, Special Publications. 2018 ; 478( 1): 217-239.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1144/sp478.3
    • Vancouver

      Hyppolito TN, Cambeses A, Angiboust S, Raimondo T, García-Casco A, Juliani C. Rehydration of eclogites and garnet-replacement processes during exhumation in the amphibolite facies [Internet]. Geological Society, London, Special Publications. 2018 ; 478( 1): 217-239.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1144/sp478.3
  • Source: Gondwana research. Unidade: IGC

    Subjects: METAMORFISMO, GEOTECTÔNICA, GEOTERMOBAROMETRIA, JURÁSSICO

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      ANGIBOUST, Samuel et al. Hot subduction in the middle Jurassic and partial melting of oceanic crust in Chilean Patagonia. Gondwana research, v. 42, p. 104-125, 2017Tradução . . Disponível em: https://doi.org/10.1016/j.gr.2016.10.007. Acesso em: 29 jun. 2024.
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      Angiboust, S., Hyppolito, T. N., Glodny, J., Cambeses, A., García-Casco, A., Calderón, M., & Juliani, C. (2017). Hot subduction in the middle Jurassic and partial melting of oceanic crust in Chilean Patagonia. Gondwana research, 42, 104-125. doi:10.1016/j.gr.2016.10.007
    • NLM

      Angiboust S, Hyppolito TN, Glodny J, Cambeses A, García-Casco A, Calderón M, Juliani C. Hot subduction in the middle Jurassic and partial melting of oceanic crust in Chilean Patagonia [Internet]. Gondwana research. 2017 ; 42 104-125.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1016/j.gr.2016.10.007
    • Vancouver

      Angiboust S, Hyppolito TN, Glodny J, Cambeses A, García-Casco A, Calderón M, Juliani C. Hot subduction in the middle Jurassic and partial melting of oceanic crust in Chilean Patagonia [Internet]. Gondwana research. 2017 ; 42 104-125.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1016/j.gr.2016.10.007
  • Source: Lithos. Unidade: IGC

    Subjects: METAMORFISMO, EVOLUÇÃO TECTÔNICA, GEOTERMOBAROMETRIA, CRETÁCEO

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      HYPPOLITO, Thaís Nogueira et al. Eclogite-, amphibolite- and blueschist-facies rocks from Diego de Almagro Island (Patagonia): episodic accretion and thermal evolution of the Chilean subduction interface during the Cretaceous. Lithos, v. 264, p. 422-440, 2016Tradução . . Disponível em: https://doi.org/10.1016/j.lithos.2016.09.001. Acesso em: 29 jun. 2024.
    • APA

      Hyppolito, T. N., Angiboust, S., Juliani, C., Glodny, J., García-Casco, A., Calderón, M., & Chopin, C. (2016). Eclogite-, amphibolite- and blueschist-facies rocks from Diego de Almagro Island (Patagonia): episodic accretion and thermal evolution of the Chilean subduction interface during the Cretaceous. Lithos, 264, 422-440. doi:10.1016/j.lithos.2016.09.001
    • NLM

      Hyppolito TN, Angiboust S, Juliani C, Glodny J, García-Casco A, Calderón M, Chopin C. Eclogite-, amphibolite- and blueschist-facies rocks from Diego de Almagro Island (Patagonia): episodic accretion and thermal evolution of the Chilean subduction interface during the Cretaceous [Internet]. Lithos. 2016 ; 264 422-440.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1016/j.lithos.2016.09.001
    • Vancouver

      Hyppolito TN, Angiboust S, Juliani C, Glodny J, García-Casco A, Calderón M, Chopin C. Eclogite-, amphibolite- and blueschist-facies rocks from Diego de Almagro Island (Patagonia): episodic accretion and thermal evolution of the Chilean subduction interface during the Cretaceous [Internet]. Lithos. 2016 ; 264 422-440.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1016/j.lithos.2016.09.001
  • Source: Journal of Metamorphic Geology. Unidades: IGC, IAG

    Subjects: METAMORFISMO, PALEOZOICO

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    • ABNT

      HYPPOLITO, Thais Nogueira et al. LP/HT metamorphism as a temporal marker of change of deformation style within the Late Palaeozoic accretionary wedge of central Chile. Journal of Metamorphic Geology, v. 33, n. 9, p. 1003-1024, 2015Tradução . . Disponível em: https://doi.org/10.1111/jmg.12166. Acesso em: 29 jun. 2024.
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      Hyppolito, T. N., Juliani, C., García-Casco, A., Meira, V. T., Bustamante, A., & Hall, C. (2015). LP/HT metamorphism as a temporal marker of change of deformation style within the Late Palaeozoic accretionary wedge of central Chile. Journal of Metamorphic Geology, 33( 9), 1003-1024. doi:10.1111/jmg.12166
    • NLM

      Hyppolito TN, Juliani C, García-Casco A, Meira VT, Bustamante A, Hall C. LP/HT metamorphism as a temporal marker of change of deformation style within the Late Palaeozoic accretionary wedge of central Chile [Internet]. Journal of Metamorphic Geology. 2015 ; 33( 9): 1003-1024.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1111/jmg.12166
    • Vancouver

      Hyppolito TN, Juliani C, García-Casco A, Meira VT, Bustamante A, Hall C. LP/HT metamorphism as a temporal marker of change of deformation style within the Late Palaeozoic accretionary wedge of central Chile [Internet]. Journal of Metamorphic Geology. 2015 ; 33( 9): 1003-1024.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1111/jmg.12166
  • Source: Terra Nova. Unidades: IGC, IAG

    Subjects: GEOTECTÔNICA, OROGÊNESE, NEOPROTEROZOICO, GONDWANA

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      MEIRA, Vinícius Tieppo et al. The role of intracontinental deformation in supercontinent assembly: insights from the Ribeira Belt, Southeastern Brazil (Neoproterozoic West Gondwana). Terra Nova, v. 27, n. 3, p. 206-217, 2015Tradução . . Disponível em: https://doi.org/10.1111/ter.12149. Acesso em: 29 jun. 2024.
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      Meira, V. T., García-Casco, A., Juliani, C., Almeida, R. P. de, & Schorscher, J. H. D. (2015). The role of intracontinental deformation in supercontinent assembly: insights from the Ribeira Belt, Southeastern Brazil (Neoproterozoic West Gondwana). Terra Nova, 27( 3), 206-217. doi:10.1111/ter.12149
    • NLM

      Meira VT, García-Casco A, Juliani C, Almeida RP de, Schorscher JHD. The role of intracontinental deformation in supercontinent assembly: insights from the Ribeira Belt, Southeastern Brazil (Neoproterozoic West Gondwana) [Internet]. Terra Nova. 2015 ; 27( 3): 206-217.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1111/ter.12149
    • Vancouver

      Meira VT, García-Casco A, Juliani C, Almeida RP de, Schorscher JHD. The role of intracontinental deformation in supercontinent assembly: insights from the Ribeira Belt, Southeastern Brazil (Neoproterozoic West Gondwana) [Internet]. Terra Nova. 2015 ; 27( 3): 206-217.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1111/ter.12149
  • Source: [Abstracts volume]. Conference titles: Hutton Symposium on Granites and Related Rocks. Unidades: IGC, IAG

    Subjects: MAGMATISMO, GEOCRONOLOGIA, GEOQUÍMICA, GONDWANA

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      MEIRA, Vinícius Tieppo et al. New geochemical and geochronological data from Ediacaran magmatism in Central Ribeira Belt, southeastern Brazil: implications for the assembly of West Gondwana. 2015, Anais.. Florianópolis: Instituto de Geociências, Universidade de São Paulo, 2015. Disponível em: http://sbg.sitepessoal.com/anais_digitalizados/internacionais/hutton%2015.pdf. Acesso em: 29 jun. 2024.
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      Meira, V. T., Schorscher, J. H. D., Juliani, C., & García-Casco, A. (2015). New geochemical and geochronological data from Ediacaran magmatism in Central Ribeira Belt, southeastern Brazil: implications for the assembly of West Gondwana. In [Abstracts volume]. Florianópolis: Instituto de Geociências, Universidade de São Paulo. Recuperado de http://sbg.sitepessoal.com/anais_digitalizados/internacionais/hutton%2015.pdf
    • NLM

      Meira VT, Schorscher JHD, Juliani C, García-Casco A. New geochemical and geochronological data from Ediacaran magmatism in Central Ribeira Belt, southeastern Brazil: implications for the assembly of West Gondwana [Internet]. [Abstracts volume]. 2015 ;[citado 2024 jun. 29 ] Available from: http://sbg.sitepessoal.com/anais_digitalizados/internacionais/hutton%2015.pdf
    • Vancouver

      Meira VT, Schorscher JHD, Juliani C, García-Casco A. New geochemical and geochronological data from Ediacaran magmatism in Central Ribeira Belt, southeastern Brazil: implications for the assembly of West Gondwana [Internet]. [Abstracts volume]. 2015 ;[citado 2024 jun. 29 ] Available from: http://sbg.sitepessoal.com/anais_digitalizados/internacionais/hutton%2015.pdf
  • Source: International Geology Review. Unidade: IGC

    Subjects: TECTÔNICA DE PLACAS, GONDWANA, GEOQUÍMICA DAS ROCHAS

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      HYPPOLITO, Thaís Nogueira et al. The nature of the Palaeozoic oceanic basin at the southwestern margin of Gondwana and implications for the origin of the Chilenia terrane (Pichilemu region, central Chile). International Geology Review, v. 56, n. 9, p. 1097-1121, 2014Tradução . . Disponível em: https://doi.org/10.1080/00206814.2014.919612. Acesso em: 29 jun. 2024.
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      Hyppolito, T. N., Juliani, C., García-Casco, A., Meira, V. T., Bustamante Londoño, A., & Hervé, F. (2014). The nature of the Palaeozoic oceanic basin at the southwestern margin of Gondwana and implications for the origin of the Chilenia terrane (Pichilemu region, central Chile). International Geology Review, 56( 9), 1097-1121. doi:10.1080/00206814.2014.919612
    • NLM

      Hyppolito TN, Juliani C, García-Casco A, Meira VT, Bustamante Londoño A, Hervé F. The nature of the Palaeozoic oceanic basin at the southwestern margin of Gondwana and implications for the origin of the Chilenia terrane (Pichilemu region, central Chile) [Internet]. International Geology Review. 2014 ; 56( 9): 1097-1121.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1080/00206814.2014.919612
    • Vancouver

      Hyppolito TN, Juliani C, García-Casco A, Meira VT, Bustamante Londoño A, Hervé F. The nature of the Palaeozoic oceanic basin at the southwestern margin of Gondwana and implications for the origin of the Chilenia terrane (Pichilemu region, central Chile) [Internet]. International Geology Review. 2014 ; 56( 9): 1097-1121.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1080/00206814.2014.919612
  • Source: Lithos. Unidade: IGC

    Subjects: METAMORFISMO, GONDWANA

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      HYPPOLITO, Thais Nogueira et al. Late Paleozoic onset of subduction and exhumation at the western margin of Gondwana (Chilenia Terrane): counterclockwise P–T paths and timing of metamorphism of deep-seated garnet–mica schist and amphibolite of Punta Sirena, Coastal Accretionary Complex, central Chile (34° S). Lithos, v. 206-207, p. 409-434, 2014Tradução . . Disponível em: https://doi.org/10.1016/j.lithos.2014.07.023. Acesso em: 29 jun. 2024.
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      Hyppolito, T. N., García-Casco, A., Juliani, C., Meira, V. T., & Hall, C. (2014). Late Paleozoic onset of subduction and exhumation at the western margin of Gondwana (Chilenia Terrane): counterclockwise P–T paths and timing of metamorphism of deep-seated garnet–mica schist and amphibolite of Punta Sirena, Coastal Accretionary Complex, central Chile (34° S). Lithos, 206-207, 409-434. doi:10.1016/j.lithos.2014.07.023
    • NLM

      Hyppolito TN, García-Casco A, Juliani C, Meira VT, Hall C. Late Paleozoic onset of subduction and exhumation at the western margin of Gondwana (Chilenia Terrane): counterclockwise P–T paths and timing of metamorphism of deep-seated garnet–mica schist and amphibolite of Punta Sirena, Coastal Accretionary Complex, central Chile (34° S) [Internet]. Lithos. 2014 ; 206-207 409-434.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1016/j.lithos.2014.07.023
    • Vancouver

      Hyppolito TN, García-Casco A, Juliani C, Meira VT, Hall C. Late Paleozoic onset of subduction and exhumation at the western margin of Gondwana (Chilenia Terrane): counterclockwise P–T paths and timing of metamorphism of deep-seated garnet–mica schist and amphibolite of Punta Sirena, Coastal Accretionary Complex, central Chile (34° S) [Internet]. Lithos. 2014 ; 206-207 409-434.[citado 2024 jun. 29 ] Available from: https://doi.org/10.1016/j.lithos.2014.07.023

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