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  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: METAMORFISMO, GRANULITO, GEOTERMOBAROMETRIA

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    • ABNT

      SILVA, Otavio Sant’ Anna G. et al. Using two-pyroxene mafic granulites to reconstruct ultra-high temperatures and the retrograde P–T path of metamorphism in the Socorro-Guaxupé Nappe (Southern Brasília Orogen, SE Brazil). International Journal of Earth Sciences, v. 113, n. , p. 161-184, 2024Tradução . . Disponível em: https://doi.org/10.1007/s00531-023-02361-y. Acesso em: 04 dez. 2025.
    • APA

      Silva, O. S. ’ A. G., Luvizotto, G. L., Fumes, R. A., Moraes, R. de, Clemence Junior, G. W., & Oliveira, M. A. F. (2024). Using two-pyroxene mafic granulites to reconstruct ultra-high temperatures and the retrograde P–T path of metamorphism in the Socorro-Guaxupé Nappe (Southern Brasília Orogen, SE Brazil). International Journal of Earth Sciences, 113( ), 161-184. doi:10.1007/s00531-023-02361-y
    • NLM

      Silva OS’ AG, Luvizotto GL, Fumes RA, Moraes R de, Clemence Junior GW, Oliveira MAF. Using two-pyroxene mafic granulites to reconstruct ultra-high temperatures and the retrograde P–T path of metamorphism in the Socorro-Guaxupé Nappe (Southern Brasília Orogen, SE Brazil) [Internet]. International Journal of Earth Sciences. 2024 ; 113( ): 161-184.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-023-02361-y
    • Vancouver

      Silva OS’ AG, Luvizotto GL, Fumes RA, Moraes R de, Clemence Junior GW, Oliveira MAF. Using two-pyroxene mafic granulites to reconstruct ultra-high temperatures and the retrograde P–T path of metamorphism in the Socorro-Guaxupé Nappe (Southern Brasília Orogen, SE Brazil) [Internet]. International Journal of Earth Sciences. 2024 ; 113( ): 161-184.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-023-02361-y
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: OROGÊNESE, GEOQUÍMICA

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    • ABNT

      SIEGESMUND, Siegfried et al. Cadomian to Cenerian accretionary orogenic processes in the Alpine basement: the detrital zircon archive. International Journal of Earth Sciences, v. 112, n. , p. 1157-1174-, 2023Tradução . . Disponível em: https://doi.org/10.1007/s00531-023-02305-6. Acesso em: 04 dez. 2025.
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      Siegesmund, S., Oriolo, S., Broge, A. S., Hueck, M., Lammerer, B., Basei, M. A. S., & Schulz, B. (2023). Cadomian to Cenerian accretionary orogenic processes in the Alpine basement: the detrital zircon archive. International Journal of Earth Sciences, 112( ), 1157-1174-. doi:10.1007/s00531-023-02305-6
    • NLM

      Siegesmund S, Oriolo S, Broge AS, Hueck M, Lammerer B, Basei MAS, Schulz B. Cadomian to Cenerian accretionary orogenic processes in the Alpine basement: the detrital zircon archive [Internet]. International Journal of Earth Sciences. 2023 ; 112( ): 1157-1174-.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-023-02305-6
    • Vancouver

      Siegesmund S, Oriolo S, Broge AS, Hueck M, Lammerer B, Basei MAS, Schulz B. Cadomian to Cenerian accretionary orogenic processes in the Alpine basement: the detrital zircon archive [Internet]. International Journal of Earth Sciences. 2023 ; 112( ): 1157-1174-.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-023-02305-6
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: GEOQUÍMICA ISOTÓPICA, PERIDOTITO

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      ALMEIDA, Vidyã Vieira et al. Composition and thermal evolution of the lithospheric mantle beneath the Ribeira Belt, SE Brazil: evidence from spinel peridotite xenoliths. International Journal of Earth Sciences, n. , p. , 2022Tradução . . Disponível em: https://doi.org/10.1007/s00531-022-02171-8. Acesso em: 04 dez. 2025.
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      Almeida, V. V., Janasi, V. de A., Faleiros, F. M., Simonetti, A., & Moraes, R. de. (2022). Composition and thermal evolution of the lithospheric mantle beneath the Ribeira Belt, SE Brazil: evidence from spinel peridotite xenoliths. International Journal of Earth Sciences, ( ), . doi:10.1007/s00531-022-02171-8
    • NLM

      Almeida VV, Janasi V de A, Faleiros FM, Simonetti A, Moraes R de. Composition and thermal evolution of the lithospheric mantle beneath the Ribeira Belt, SE Brazil: evidence from spinel peridotite xenoliths [Internet]. International Journal of Earth Sciences. 2022 ;( ): .[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-022-02171-8
    • Vancouver

      Almeida VV, Janasi V de A, Faleiros FM, Simonetti A, Moraes R de. Composition and thermal evolution of the lithospheric mantle beneath the Ribeira Belt, SE Brazil: evidence from spinel peridotite xenoliths [Internet]. International Journal of Earth Sciences. 2022 ;( ): .[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-022-02171-8
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: GEOCRONOLOGIA, ZIRCÃO, NEOPROTEROZOICO

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    • ABNT

      SILVA LARA, Hernán et al. Reassessing the polyphase Neoproterozoic evolution of the Punta del Este Terrane, Dom Feliciano Belt, Uruguay. International Journal of Earth Sciences, v. 111, n. , p. 2283-2316-, 2022Tradução . . Disponível em: https://doi.org/10.1007/s00531-022-02230-0. Acesso em: 04 dez. 2025.
    • APA

      Silva Lara, H., Siegesmund, S., Oriolo, S., Hueck, M., Wemmer, K., Basei, M. A. S., & Oyhantçabal, P. (2022). Reassessing the polyphase Neoproterozoic evolution of the Punta del Este Terrane, Dom Feliciano Belt, Uruguay. International Journal of Earth Sciences, 111( ), 2283-2316-. doi:10.1007/s00531-022-02230-0
    • NLM

      Silva Lara H, Siegesmund S, Oriolo S, Hueck M, Wemmer K, Basei MAS, Oyhantçabal P. Reassessing the polyphase Neoproterozoic evolution of the Punta del Este Terrane, Dom Feliciano Belt, Uruguay [Internet]. International Journal of Earth Sciences. 2022 ; 111( ): 2283-2316-.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-022-02230-0
    • Vancouver

      Silva Lara H, Siegesmund S, Oriolo S, Hueck M, Wemmer K, Basei MAS, Oyhantçabal P. Reassessing the polyphase Neoproterozoic evolution of the Punta del Este Terrane, Dom Feliciano Belt, Uruguay [Internet]. International Journal of Earth Sciences. 2022 ; 111( ): 2283-2316-.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-022-02230-0
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: GRANULITO, GEOTERMOBAROMETRIA

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    • ABNT

      HERNANDEZ TASCO, Lizeth e MORAES, Renato de. Relation between partial melting, granulite metamorphism, crystallization, deformation of leucosome and the influence of these processes on the cooling of the root of a hot orogen. International Journal of Earth Sciences, v. 111, p. 1395-1412, 2022Tradução . . Disponível em: https://doi.org/10.1007/s00531-022-02185-2. Acesso em: 04 dez. 2025.
    • APA

      Hernandez Tasco, L., & Moraes, R. de. (2022). Relation between partial melting, granulite metamorphism, crystallization, deformation of leucosome and the influence of these processes on the cooling of the root of a hot orogen. International Journal of Earth Sciences, 111, 1395-1412. doi:10.1007/s00531-022-02185-2
    • NLM

      Hernandez Tasco L, Moraes R de. Relation between partial melting, granulite metamorphism, crystallization, deformation of leucosome and the influence of these processes on the cooling of the root of a hot orogen [Internet]. International Journal of Earth Sciences. 2022 ; 111 1395-1412.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-022-02185-2
    • Vancouver

      Hernandez Tasco L, Moraes R de. Relation between partial melting, granulite metamorphism, crystallization, deformation of leucosome and the influence of these processes on the cooling of the root of a hot orogen [Internet]. International Journal of Earth Sciences. 2022 ; 111 1395-1412.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-022-02185-2
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: ISÓTOPOS, OROGÊNESE, MAGMATISMO, PALEOGEOGRAFIA

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    • ABNT

      VESELÁ, P. et al. The detrital zircon record of Variscan to post‐Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps). International Journal of Earth Sciences, n. , p. , 2022Tradução . . Disponível em: https://doi.org/10.1007/s00531-022-02179-0. Acesso em: 04 dez. 2025.
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      Veselá, P., Oriolo, S., Basei, M. A. S., Lammerer, B., & Siegesmund, S. (2022). The detrital zircon record of Variscan to post‐Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps). International Journal of Earth Sciences, ( ), . doi:10.1007/s00531-022-02179-0
    • NLM

      Veselá P, Oriolo S, Basei MAS, Lammerer B, Siegesmund S. The detrital zircon record of Variscan to post‐Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps) [Internet]. International Journal of Earth Sciences. 2022 ;( ): .[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-022-02179-0
    • Vancouver

      Veselá P, Oriolo S, Basei MAS, Lammerer B, Siegesmund S. The detrital zircon record of Variscan to post‐Variscan tectonosedimentary and magmatic processes in the Tauern Window (Eastern Alps) [Internet]. International Journal of Earth Sciences. 2022 ;( ): .[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-022-02179-0
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: GEOCRONOLOGIA, GONDWANA, BASALTO

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      ROJO, Diego et al. The low-grade basement at Península La Carmela, Chilean Patagonia: new data for unraveling the pre-Permian basin nature of the Eastern Andean Metamorphic Complex. International Journal of Earth Sciences, v. 110, n. , p. 2021-2042, 2021Tradução . . Disponível em: https://doi.org/10.1007/s00531-021-02054-4. Acesso em: 04 dez. 2025.
    • APA

      Rojo, D., Calderón, M., Ghiglione, M. C., Suárez, R. J., Quezada, P., Cataldo, J., et al. (2021). The low-grade basement at Península La Carmela, Chilean Patagonia: new data for unraveling the pre-Permian basin nature of the Eastern Andean Metamorphic Complex. International Journal of Earth Sciences, 110( ), 2021-2042. doi:10.1007/s00531-021-02054-4
    • NLM

      Rojo D, Calderón M, Ghiglione MC, Suárez RJ, Quezada P, Cataldo J, Hervé F, Charrier R, Galaz G, Suárez M, Guettner G, Babinski M. The low-grade basement at Península La Carmela, Chilean Patagonia: new data for unraveling the pre-Permian basin nature of the Eastern Andean Metamorphic Complex [Internet]. International Journal of Earth Sciences. 2021 ; 110( ): 2021-2042.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-021-02054-4
    • Vancouver

      Rojo D, Calderón M, Ghiglione MC, Suárez RJ, Quezada P, Cataldo J, Hervé F, Charrier R, Galaz G, Suárez M, Guettner G, Babinski M. The low-grade basement at Península La Carmela, Chilean Patagonia: new data for unraveling the pre-Permian basin nature of the Eastern Andean Metamorphic Complex [Internet]. International Journal of Earth Sciences. 2021 ; 110( ): 2021-2042.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-021-02054-4
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: METAMORFISMO, GONDWANA, GEOTECTÔNICA, PALEOZOICO

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    • ABNT

      GONZÁLEZ, Pablo D. et al. Early Paleozoic structural and metamorphic evolution of the Transpatagonian Orogen related to Gondwana assembly. International Journal of Earth Sciences, v. 110, p. 81-111, 2021Tradução . . Disponível em: https://doi.org/10.1007/s00531-020-01939-0. Acesso em: 04 dez. 2025.
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      González, P. D., Naipauer, M., Sato, A. M., Varela, R., Basei, M. A. S., Cábana, M. C., et al. (2021). Early Paleozoic structural and metamorphic evolution of the Transpatagonian Orogen related to Gondwana assembly. International Journal of Earth Sciences, 110, 81-111. doi:10.1007/s00531-020-01939-0
    • NLM

      González PD, Naipauer M, Sato AM, Varela R, Basei MAS, Cábana MC, Vlach SRF, Arce M, Parada M. Early Paleozoic structural and metamorphic evolution of the Transpatagonian Orogen related to Gondwana assembly [Internet]. International Journal of Earth Sciences. 2021 ; 110 81-111.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-020-01939-0
    • Vancouver

      González PD, Naipauer M, Sato AM, Varela R, Basei MAS, Cábana MC, Vlach SRF, Arce M, Parada M. Early Paleozoic structural and metamorphic evolution of the Transpatagonian Orogen related to Gondwana assembly [Internet]. International Journal of Earth Sciences. 2021 ; 110 81-111.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-020-01939-0
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: OROGÊNESE, EVOLUÇÃO TECTÔNICA

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    • ABNT

      SIEGESMUND, Siegfried et al. The birth of the Alps: Ediacaran to Paleozoic accretionary processes and crustal growth along the northern Gondwana margin. International Journal of Earth Sciences, n. , p. 1321-1348-, 2021Tradução . . Disponível em: https://doi.org/10.1007/s00531-021-02019-7. Acesso em: 04 dez. 2025.
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      Siegesmund, S., Oriolo, S., Schulz, B., Heinrichs, T., Basei, M. A. S., & Lammerer, B. (2021). The birth of the Alps: Ediacaran to Paleozoic accretionary processes and crustal growth along the northern Gondwana margin. International Journal of Earth Sciences, ( ), 1321-1348-. doi:10.1007/s00531-021-02019-7
    • NLM

      Siegesmund S, Oriolo S, Schulz B, Heinrichs T, Basei MAS, Lammerer B. The birth of the Alps: Ediacaran to Paleozoic accretionary processes and crustal growth along the northern Gondwana margin [Internet]. International Journal of Earth Sciences. 2021 ;( ): 1321-1348-.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-021-02019-7
    • Vancouver

      Siegesmund S, Oriolo S, Schulz B, Heinrichs T, Basei MAS, Lammerer B. The birth of the Alps: Ediacaran to Paleozoic accretionary processes and crustal growth along the northern Gondwana margin [Internet]. International Journal of Earth Sciences. 2021 ;( ): 1321-1348-.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-021-02019-7
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: GONDWANA, DEVONIANO

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    • ABNT

      ARIEL ARNOL, Jonatan et al. Provenance analysis of Devonian peripheral foreland basins in SW Gondwana, case of the Gualilán Group, Precordillera Argentina. International Journal of Earth Sciences, n. , p. -, 2020Tradução . . Disponível em: https://doi.org/10.1007/s00531-020-01914-9. Acesso em: 04 dez. 2025.
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      Ariel Arnol, J., Javier Uriz, N., Cingolani, C. A., Basei, M. A. S., & Abre, P. (2020). Provenance analysis of Devonian peripheral foreland basins in SW Gondwana, case of the Gualilán Group, Precordillera Argentina. International Journal of Earth Sciences, ( ), -. doi:10.1007/s00531-020-01914-9
    • NLM

      Ariel Arnol J, Javier Uriz N, Cingolani CA, Basei MAS, Abre P. Provenance analysis of Devonian peripheral foreland basins in SW Gondwana, case of the Gualilán Group, Precordillera Argentina [Internet]. International Journal of Earth Sciences. 2020 ;( ): -.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-020-01914-9
    • Vancouver

      Ariel Arnol J, Javier Uriz N, Cingolani CA, Basei MAS, Abre P. Provenance analysis of Devonian peripheral foreland basins in SW Gondwana, case of the Gualilán Group, Precordillera Argentina [Internet]. International Journal of Earth Sciences. 2020 ;( ): -.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-020-01914-9
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: MAGMA, GEOQUÍMICA, GEOTECTÔNICA

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      PASSARELLI, Claudia Regina e VERMA, Sanjeet Kumar. Evidence of mingling between contrasting magmas in the Ribeirão do Óleo Pluton, Coastal Terrane and the tectonic implications on the Ribeira Belt, Brazil. International Journal of Earth Sciences, n. , p. , 2020Tradução . . Disponível em: https://doi.org/10.1007/s00531-019-01804-9. Acesso em: 04 dez. 2025.
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      Passarelli, C. R., & Verma, S. K. (2020). Evidence of mingling between contrasting magmas in the Ribeirão do Óleo Pluton, Coastal Terrane and the tectonic implications on the Ribeira Belt, Brazil. International Journal of Earth Sciences, ( ), . doi:10.1007/s00531-019-01804-9
    • NLM

      Passarelli CR, Verma SK. Evidence of mingling between contrasting magmas in the Ribeirão do Óleo Pluton, Coastal Terrane and the tectonic implications on the Ribeira Belt, Brazil [Internet]. International Journal of Earth Sciences. 2020 ;( ): .[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-019-01804-9
    • Vancouver

      Passarelli CR, Verma SK. Evidence of mingling between contrasting magmas in the Ribeirão do Óleo Pluton, Coastal Terrane and the tectonic implications on the Ribeira Belt, Brazil [Internet]. International Journal of Earth Sciences. 2020 ;( ): .[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-019-01804-9
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: INTRUSÃO ÍGNEA, QUÍMICA MINERAL, GEOQUÍMICA, MAGMATISMO

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      FRANCIOSI, L. et al. Petrogenesis of the Solanas gabbro-granodiorite intrusion, Sàrrabus (southeastern Sardinia, Italy): implications for Late Variscan magmatism. International Journal of Earth Sciences, v. 108, n. 3, p. 989-1012, 2019Tradução . . Disponível em: https://doi.org/10.1007/s00531-019-01689-8. Acesso em: 04 dez. 2025.
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      Franciosi, L., D’Antonio, M., Fedele, L., Guarino, V., Tassinari, C. C. G., De Gennaro, R., & Cucciniello, C. (2019). Petrogenesis of the Solanas gabbro-granodiorite intrusion, Sàrrabus (southeastern Sardinia, Italy): implications for Late Variscan magmatism. International Journal of Earth Sciences, 108( 3), 989-1012. doi:10.1007/s00531-019-01689-8
    • NLM

      Franciosi L, D’Antonio M, Fedele L, Guarino V, Tassinari CCG, De Gennaro R, Cucciniello C. Petrogenesis of the Solanas gabbro-granodiorite intrusion, Sàrrabus (southeastern Sardinia, Italy): implications for Late Variscan magmatism [Internet]. International Journal of Earth Sciences. 2019 ; 108( 3): 989-1012.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-019-01689-8
    • Vancouver

      Franciosi L, D’Antonio M, Fedele L, Guarino V, Tassinari CCG, De Gennaro R, Cucciniello C. Petrogenesis of the Solanas gabbro-granodiorite intrusion, Sàrrabus (southeastern Sardinia, Italy): implications for Late Variscan magmatism [Internet]. International Journal of Earth Sciences. 2019 ; 108( 3): 989-1012.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-019-01689-8
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: GONDWANA, CISALHAMENTO

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      HUECK, Mathias et al. Evolution of the Major Gercino Shear Zone in the Dom Feliciano Belt, South Brazil, and implications for the assembly of southwestern Gondwana. International Journal of Earth Sciences, v. 108, n. , p. 403-425, 2018Tradução . . Disponível em: https://doi.org/10.1007/s00531-018-1660-4. Acesso em: 04 dez. 2025.
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      Hueck, M., Basei, M. A. S., Wemmer, K., Oriolo, S., Heidelbach, F., & Siegesmund, S. (2018). Evolution of the Major Gercino Shear Zone in the Dom Feliciano Belt, South Brazil, and implications for the assembly of southwestern Gondwana. International Journal of Earth Sciences, 108( ), 403-425. doi:10.1007/s00531-018-1660-4
    • NLM

      Hueck M, Basei MAS, Wemmer K, Oriolo S, Heidelbach F, Siegesmund S. Evolution of the Major Gercino Shear Zone in the Dom Feliciano Belt, South Brazil, and implications for the assembly of southwestern Gondwana [Internet]. International Journal of Earth Sciences. 2018 ; 108( ): 403-425.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-018-1660-4
    • Vancouver

      Hueck M, Basei MAS, Wemmer K, Oriolo S, Heidelbach F, Siegesmund S. Evolution of the Major Gercino Shear Zone in the Dom Feliciano Belt, South Brazil, and implications for the assembly of southwestern Gondwana [Internet]. International Journal of Earth Sciences. 2018 ; 108( ): 403-425.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-018-1660-4
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: GEOCRONOLOGIA, GEODINÂMICA, MAGMATISMO

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      DAHLQUIST, Juan et al. Petrological, geochemical, isotopic, and geochronological constraints for the Late Devonian–Early Carboniferous magmatism in SW Gondwana (27–32°LS): an example of geodynamic switching. International Journal of Earth Sciences, v. 107, n. 7, p. 2575-2603, 2018Tradução . . Disponível em: https://doi.org/10.1007/s00531-018-1615-9. Acesso em: 04 dez. 2025.
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      Dahlquist, J., Alasino, P., Basei, M. A. S., Morales Cámera, M. M., Macchioli Grande, M., & Campos Neto, M. da C. (2018). Petrological, geochemical, isotopic, and geochronological constraints for the Late Devonian–Early Carboniferous magmatism in SW Gondwana (27–32°LS): an example of geodynamic switching. International Journal of Earth Sciences, 107( 7), 2575-2603. doi:10.1007/s00531-018-1615-9
    • NLM

      Dahlquist J, Alasino P, Basei MAS, Morales Cámera MM, Macchioli Grande M, Campos Neto M da C. Petrological, geochemical, isotopic, and geochronological constraints for the Late Devonian–Early Carboniferous magmatism in SW Gondwana (27–32°LS): an example of geodynamic switching [Internet]. International Journal of Earth Sciences. 2018 ; 107( 7): 2575-2603.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-018-1615-9
    • Vancouver

      Dahlquist J, Alasino P, Basei MAS, Morales Cámera MM, Macchioli Grande M, Campos Neto M da C. Petrological, geochemical, isotopic, and geochronological constraints for the Late Devonian–Early Carboniferous magmatism in SW Gondwana (27–32°LS): an example of geodynamic switching [Internet]. International Journal of Earth Sciences. 2018 ; 107( 7): 2575-2603.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-018-1615-9
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: GONDWANA, SEDIMENTOLOGIA, ZIRCÃO, CAMBRIANO, ORDOVICIANO

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    • ABNT

      SIEGESMUND, Siegfried et al. Provenance of Austroalpine basement metasediments: tightening up Early Palaeozoic connections between peri-Gondwanan domains of central Europe and Northern Africa. International Journal of Earth Sciences, v. 107, n. 6, p. 2293-2315, 2018Tradução . . Disponível em: https://doi.org/10.1007/s00531-018-1599-5. Acesso em: 04 dez. 2025.
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      Siegesmund, S., Oriolo, S., Heinrichs, T., Basei, M. A. S., Nolte, N., Hüttenrauch, F., & Schulz, B. (2018). Provenance of Austroalpine basement metasediments: tightening up Early Palaeozoic connections between peri-Gondwanan domains of central Europe and Northern Africa. International Journal of Earth Sciences, 107( 6), 2293-2315. doi:10.1007/s00531-018-1599-5
    • NLM

      Siegesmund S, Oriolo S, Heinrichs T, Basei MAS, Nolte N, Hüttenrauch F, Schulz B. Provenance of Austroalpine basement metasediments: tightening up Early Palaeozoic connections between peri-Gondwanan domains of central Europe and Northern Africa [Internet]. International Journal of Earth Sciences. 2018 ; 107( 6): 2293-2315.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-018-1599-5
    • Vancouver

      Siegesmund S, Oriolo S, Heinrichs T, Basei MAS, Nolte N, Hüttenrauch F, Schulz B. Provenance of Austroalpine basement metasediments: tightening up Early Palaeozoic connections between peri-Gondwanan domains of central Europe and Northern Africa [Internet]. International Journal of Earth Sciences. 2018 ; 107( 6): 2293-2315.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-018-1599-5
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: METAMORFISMO, NAPPE

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      MOTTA, Rafael Gonçalves da e MORAES, Renato de. Pseudo- and real-inverted metamorphism caused by the superposition and extrusion of a stack of nappes: a case study of the Southern Brasília Orogen, Brazil. International Journal of Earth Sciences, v. 106, n. 7, p. 2407-2427, 2017Tradução . . Disponível em: https://doi.org/10.1007/s00531-016-1436-7. Acesso em: 04 dez. 2025.
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      Motta, R. G. da, & Moraes, R. de. (2017). Pseudo- and real-inverted metamorphism caused by the superposition and extrusion of a stack of nappes: a case study of the Southern Brasília Orogen, Brazil. International Journal of Earth Sciences, 106( 7), 2407-2427. doi:10.1007/s00531-016-1436-7
    • NLM

      Motta RG da, Moraes R de. Pseudo- and real-inverted metamorphism caused by the superposition and extrusion of a stack of nappes: a case study of the Southern Brasília Orogen, Brazil [Internet]. International Journal of Earth Sciences. 2017 ; 106( 7): 2407-2427.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-016-1436-7
    • Vancouver

      Motta RG da, Moraes R de. Pseudo- and real-inverted metamorphism caused by the superposition and extrusion of a stack of nappes: a case study of the Southern Brasília Orogen, Brazil [Internet]. International Journal of Earth Sciences. 2017 ; 106( 7): 2407-2427.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-016-1436-7
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: ROCHAS MAGMÁTICAS, GEOQUÍMICA, PETROGRAFIA

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      GUARINO, Vincenza et al. U–Pb ages, geochemistry, C–O–Nd–Sr–Hf isotopes and petrogenesis of the Catalão II carbonatitic complex (Alto Paranaíba Igneous Province, Brazil): implications for regional-scale heterogeneities in the Brazilian carbonatite associations. International Journal of Earth Sciences, v. 106, n. 6, p. 1963-1989, 2017Tradução . . Disponível em: https://doi.org/10.1007/s00531-016-1402-4. Acesso em: 04 dez. 2025.
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      Guarino, V., Wu, F. -Y., Melluso, L., Gomes, C. B., Tassinari, C. C. G., Ruberti, E., & Brilli, M. (2017). U–Pb ages, geochemistry, C–O–Nd–Sr–Hf isotopes and petrogenesis of the Catalão II carbonatitic complex (Alto Paranaíba Igneous Province, Brazil): implications for regional-scale heterogeneities in the Brazilian carbonatite associations. International Journal of Earth Sciences, 106( 6), 1963-1989. doi:10.1007/s00531-016-1402-4
    • NLM

      Guarino V, Wu F-Y, Melluso L, Gomes CB, Tassinari CCG, Ruberti E, Brilli M. U–Pb ages, geochemistry, C–O–Nd–Sr–Hf isotopes and petrogenesis of the Catalão II carbonatitic complex (Alto Paranaíba Igneous Province, Brazil): implications for regional-scale heterogeneities in the Brazilian carbonatite associations [Internet]. International Journal of Earth Sciences. 2017 ; 106( 6): 1963-1989.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-016-1402-4
    • Vancouver

      Guarino V, Wu F-Y, Melluso L, Gomes CB, Tassinari CCG, Ruberti E, Brilli M. U–Pb ages, geochemistry, C–O–Nd–Sr–Hf isotopes and petrogenesis of the Catalão II carbonatitic complex (Alto Paranaíba Igneous Province, Brazil): implications for regional-scale heterogeneities in the Brazilian carbonatite associations [Internet]. International Journal of Earth Sciences. 2017 ; 106( 6): 1963-1989.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-016-1402-4
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: ZIRCÃO, GEOCRONOLOGIA, SEDIMENTOLOGIA, CRETÁCEO

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      DINIS, Pedro A et al. Detrital zircon geochronology of the Cretaceous succession from the Iberian Atlantic Margin: palaeogeographic implications. International Journal of Earth Sciences, v. 105, n. 3, p. 727-745, 2016Tradução . . Disponível em: https://doi.org/10.1007/s00531-015-1221-z. Acesso em: 04 dez. 2025.
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      Dinis, P. A., Dinis, J., Tassinari, C. C. G., Carter, A., Callapez, P., & Morais, M. (2016). Detrital zircon geochronology of the Cretaceous succession from the Iberian Atlantic Margin: palaeogeographic implications. International Journal of Earth Sciences, 105( 3), 727-745. doi:10.1007/s00531-015-1221-z
    • NLM

      Dinis PA, Dinis J, Tassinari CCG, Carter A, Callapez P, Morais M. Detrital zircon geochronology of the Cretaceous succession from the Iberian Atlantic Margin: palaeogeographic implications [Internet]. International Journal of Earth Sciences. 2016 ; 105( 3): 727-745.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-015-1221-z
    • Vancouver

      Dinis PA, Dinis J, Tassinari CCG, Carter A, Callapez P, Morais M. Detrital zircon geochronology of the Cretaceous succession from the Iberian Atlantic Margin: palaeogeographic implications [Internet]. International Journal of Earth Sciences. 2016 ; 105( 3): 727-745.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-015-1221-z
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: GEOCRONOLOGIA, GEOQUÍMICA, ISÓTOPOS, MAGMATISMO

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      DAHLQUIST, Juan et al. The Capilla del Monte pluton, Sierras de Córdoba, Argentina: the easternmost Early Carboniferous magmatism in the pre-Andean SW Gondwana margin. International Journal of Earth Sciences, v. 105, n. 5, p. 1287-1305, 2015Tradução . . Disponível em: https://doi.org/10.1007/s00531-015-1249-0. Acesso em: 04 dez. 2025.
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      Dahlquist, J., Pankhurst, R. J., Rapela, C. W., Basei, M. A. S., Alasino, P., Saavedra, J., et al. (2015). The Capilla del Monte pluton, Sierras de Córdoba, Argentina: the easternmost Early Carboniferous magmatism in the pre-Andean SW Gondwana margin. International Journal of Earth Sciences, 105( 5), 1287-1305. doi:10.1007/s00531-015-1249-0
    • NLM

      Dahlquist J, Pankhurst RJ, Rapela CW, Basei MAS, Alasino P, Saavedra J, Baldo EGA, Murra JA, Campos Neto M da C. The Capilla del Monte pluton, Sierras de Córdoba, Argentina: the easternmost Early Carboniferous magmatism in the pre-Andean SW Gondwana margin [Internet]. International Journal of Earth Sciences. 2015 ; 105( 5): 1287-1305.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-015-1249-0
    • Vancouver

      Dahlquist J, Pankhurst RJ, Rapela CW, Basei MAS, Alasino P, Saavedra J, Baldo EGA, Murra JA, Campos Neto M da C. The Capilla del Monte pluton, Sierras de Córdoba, Argentina: the easternmost Early Carboniferous magmatism in the pre-Andean SW Gondwana margin [Internet]. International Journal of Earth Sciences. 2015 ; 105( 5): 1287-1305.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-015-1249-0
  • Fonte: International Journal of Earth Sciences. Unidade: IGC

    Assuntos: GEOCRONOLOGIA, ZIRCÃO, ROCHAS GRANÍTICAS

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      SALAZAR, Carlos Alejandro et al. Age and magnetic fabric of the Três Córregos granite batholith: evidence for Ediacaran transtension in the Ribeira Belt (SE Brazil). International Journal of Earth Sciences, v. 102, n. 6, p. 1563-1581, 2013Tradução . . Disponível em: https://doi.org/10.1007/s00531-013-0908-2. Acesso em: 04 dez. 2025.
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      Salazar, C. A., Archanjo, C. J., Rodrigues, S. W. de O., Hollanda, M. H. B. M. de, & Liu, D. (2013). Age and magnetic fabric of the Três Córregos granite batholith: evidence for Ediacaran transtension in the Ribeira Belt (SE Brazil). International Journal of Earth Sciences, 102( 6), 1563-1581. doi:10.1007/s00531-013-0908-2
    • NLM

      Salazar CA, Archanjo CJ, Rodrigues SW de O, Hollanda MHBM de, Liu D. Age and magnetic fabric of the Três Córregos granite batholith: evidence for Ediacaran transtension in the Ribeira Belt (SE Brazil) [Internet]. International Journal of Earth Sciences. 2013 ; 102( 6): 1563-1581.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-013-0908-2
    • Vancouver

      Salazar CA, Archanjo CJ, Rodrigues SW de O, Hollanda MHBM de, Liu D. Age and magnetic fabric of the Três Córregos granite batholith: evidence for Ediacaran transtension in the Ribeira Belt (SE Brazil) [Internet]. International Journal of Earth Sciences. 2013 ; 102( 6): 1563-1581.[citado 2025 dez. 04 ] Available from: https://doi.org/10.1007/s00531-013-0908-2

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