Filtros : "García-Casco, Antonio" Limpar

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  • 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: 05 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. 05 ] 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. 05 ] Available from: https://doi.org/10.1144/sp478.3
  • Source: Gondwana research. Unidade: IGC

    Subjects: METAMORFISMO, GEOTECTÔNICA, GEOTERMOBAROMETRIA, JURÁSSICO

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    • ABNT

      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: 05 jun. 2024.
    • APA

      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. 05 ] 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. 05 ] 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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    • ABNT

      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: 05 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. 05 ] 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. 05 ] 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: 05 jun. 2024.
    • APA

      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. 05 ] 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. 05 ] Available from: https://doi.org/10.1111/jmg.12166
  • Source: Terra Nova. Unidades: IGC, IAG

    Subjects: GEOTECTÔNICA, OROGÊNESE, NEOPROTEROZOICO, GONDWANA

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    • ABNT

      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: 05 jun. 2024.
    • APA

      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. 05 ] 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. 05 ] Available from: https://doi.org/10.1111/ter.12149
  • Source: Anais. Conference titles: Simpósio Nacional de Estudos Tectônicos. Unidades: IGC, IAG

    Subjects: GEOLOGIA ESTRUTURAL, GEOTECTÔNICA, OROGÊNESE

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    • ABNT

      MEIRA, Vinícius Tieppo et al. The Ribeira Belt and the role of intracontinental deformation in the supercontinent assembly:: a new hypothesis to be tested. 2015, Anais.. [Vitória]: Instituto de Geociências, Universidade de São Paulo, 2015. Disponível em: https://repositorio.usp.br/directbitstream/ae5a2dbb-9806-49ca-ad84-c9d17d98f286/2695168.pdf. Acesso em: 05 jun. 2024.
    • APA

      Meira, V. T., Juliani, C., Schorscher, J. H. D., Almeida, R. P. de, Hyppolito, T. N., García-Casco, A., & Fossen, H. (2015). The Ribeira Belt and the role of intracontinental deformation in the supercontinent assembly:: a new hypothesis to be tested. In Anais. [Vitória]: Instituto de Geociências, Universidade de São Paulo. Recuperado de https://repositorio.usp.br/directbitstream/ae5a2dbb-9806-49ca-ad84-c9d17d98f286/2695168.pdf
    • NLM

      Meira VT, Juliani C, Schorscher JHD, Almeida RP de, Hyppolito TN, García-Casco A, Fossen H. The Ribeira Belt and the role of intracontinental deformation in the supercontinent assembly:: a new hypothesis to be tested [Internet]. Anais. 2015 ;[citado 2024 jun. 05 ] Available from: https://repositorio.usp.br/directbitstream/ae5a2dbb-9806-49ca-ad84-c9d17d98f286/2695168.pdf
    • Vancouver

      Meira VT, Juliani C, Schorscher JHD, Almeida RP de, Hyppolito TN, García-Casco A, Fossen H. The Ribeira Belt and the role of intracontinental deformation in the supercontinent assembly:: a new hypothesis to be tested [Internet]. Anais. 2015 ;[citado 2024 jun. 05 ] Available from: https://repositorio.usp.br/directbitstream/ae5a2dbb-9806-49ca-ad84-c9d17d98f286/2695168.pdf
  • 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: 05 jun. 2024.
    • APA

      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. 05 ] 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. 05 ] Available from: http://sbg.sitepessoal.com/anais_digitalizados/internacionais/hutton%2015.pdf
  • Source: 9th SSAGI: Program and Abstracts. Conference titles: South American Symposium on Isotope Geology. Unidade: IGC

    Subjects: NEOPROTEROZOICO, MAGMATISMO

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      MEIRA, Vinícius Tieppo et al. Does the Pico do Papagaio Batholith indeed represent a Neoproterozoic magmatic arc? 2014, Anais.. São Paulo: Instituto de Geociências - USP, 2014. Disponível em: https://repositorio.usp.br/directbitstream/765c9ca8-d7f6-4951-a970-0830062e69bc/2704466.pdf. Acesso em: 05 jun. 2024.
    • APA

      Meira, V. T., Juliani, C., Schorscher, J. H. D., García-Casco, A., & Meira, T. N. H. (2014). Does the Pico do Papagaio Batholith indeed represent a Neoproterozoic magmatic arc? In 9th SSAGI: Program and Abstracts. São Paulo: Instituto de Geociências - USP. Recuperado de https://repositorio.usp.br/directbitstream/765c9ca8-d7f6-4951-a970-0830062e69bc/2704466.pdf
    • NLM

      Meira VT, Juliani C, Schorscher JHD, García-Casco A, Meira TNH. Does the Pico do Papagaio Batholith indeed represent a Neoproterozoic magmatic arc? [Internet]. 9th SSAGI: Program and Abstracts. 2014 ;[citado 2024 jun. 05 ] Available from: https://repositorio.usp.br/directbitstream/765c9ca8-d7f6-4951-a970-0830062e69bc/2704466.pdf
    • Vancouver

      Meira VT, Juliani C, Schorscher JHD, García-Casco A, Meira TNH. Does the Pico do Papagaio Batholith indeed represent a Neoproterozoic magmatic arc? [Internet]. 9th SSAGI: Program and Abstracts. 2014 ;[citado 2024 jun. 05 ] Available from: https://repositorio.usp.br/directbitstream/765c9ca8-d7f6-4951-a970-0830062e69bc/2704466.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: 05 jun. 2024.
    • APA

      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. 05 ] 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. 05 ] 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: 05 jun. 2024.
    • APA

      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. 05 ] 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. 05 ] Available from: https://doi.org/10.1016/j.lithos.2014.07.023

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