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  • Source: Global and Planetary Change. Unidades: IAG, IO

    Assunto: MERCÚRIO (ELEMENTO QUÍMICO)

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      PERCIVAL, L. M. E. et al. Determining the style and provenance of magmatic activity during the Early Aptian Oceanic Anoxic Event (OAE 1a). Global and Planetary Change, v. 200, 2021Tradução . . Disponível em: https://doi.org/10.1016/j.gloplacha.2021.103461. Acesso em: 13 jun. 2024.
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      Percival, L. M. E., Tedeschi, L. R., Creaser, R. A., Bottini, C., Erba, E., Giraud, F., et al. (2021). Determining the style and provenance of magmatic activity during the Early Aptian Oceanic Anoxic Event (OAE 1a). Global and Planetary Change, 200. doi:10.1016/j.gloplacha.2021.103461
    • NLM

      Percival LME, Tedeschi LR, Creaser RA, Bottini C, Erba E, Giraud F, Svensen H, Savian J, Trindade RIF da, Coccioni R, Frontalini F, Jovane L, Mather TA, Jenkyns HC. Determining the style and provenance of magmatic activity during the Early Aptian Oceanic Anoxic Event (OAE 1a) [Internet]. Global and Planetary Change. 2021 ; 200[citado 2024 jun. 13 ] Available from: https://doi.org/10.1016/j.gloplacha.2021.103461
    • Vancouver

      Percival LME, Tedeschi LR, Creaser RA, Bottini C, Erba E, Giraud F, Svensen H, Savian J, Trindade RIF da, Coccioni R, Frontalini F, Jovane L, Mather TA, Jenkyns HC. Determining the style and provenance of magmatic activity during the Early Aptian Oceanic Anoxic Event (OAE 1a) [Internet]. Global and Planetary Change. 2021 ; 200[citado 2024 jun. 13 ] Available from: https://doi.org/10.1016/j.gloplacha.2021.103461
  • Source: Nature Communications. Unidade: IAG

    Subjects: GEOQUÍMICA, GEOLOGIA, PETROLOGIA, MAGMATISMO, MUDANÇA CLIMÁTICA

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      CAPRIOLO, Manfredo et al. Massive methane fluxing from magma-sediment interaction in the end-Triassic Central Atlantic Magmatic Province. Nature Communications, v. 12, 2021Tradução . . Disponível em: https://doi.org/10.1038/s41467-021-25510-w. Acesso em: 13 jun. 2024.
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      Capriolo, M., Marzoli, A., Aradi, L. E., Ackerson, M. R., Bartoli, O., Callegaro, S., et al. (2021). Massive methane fluxing from magma-sediment interaction in the end-Triassic Central Atlantic Magmatic Province. Nature Communications, 12. doi:10.1038/s41467-021-25510-w
    • NLM

      Capriolo M, Marzoli A, Aradi LE, Ackerson MR, Bartoli O, Callegaro S, Dal Corso J, Ernesto M, Vasconcellos EMG, De Min A, Newton RJ, Szabó C. Massive methane fluxing from magma-sediment interaction in the end-Triassic Central Atlantic Magmatic Province [Internet]. Nature Communications. 2021 ; 12[citado 2024 jun. 13 ] Available from: https://doi.org/10.1038/s41467-021-25510-w
    • Vancouver

      Capriolo M, Marzoli A, Aradi LE, Ackerson MR, Bartoli O, Callegaro S, Dal Corso J, Ernesto M, Vasconcellos EMG, De Min A, Newton RJ, Szabó C. Massive methane fluxing from magma-sediment interaction in the end-Triassic Central Atlantic Magmatic Province [Internet]. Nature Communications. 2021 ; 12[citado 2024 jun. 13 ] Available from: https://doi.org/10.1038/s41467-021-25510-w
  • Source: Precambrian Research. Unidade: IAG

    Subjects: PALEOMAGNETISMO, GONDWANA, CAMBRIANO

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      TEMPORIM, Filipe Altoe et al. Constraining the Cambrian drift of Gondwana with new paleomagnetic data from post-collisional plutons of the Araçuaí orogen, SE Brazil. Precambrian Research, v. 359, p. art. 106212, 2021Tradução . . Disponível em: https://doi.org/10.1016/j.precamres.2021.106212. Acesso em: 13 jun. 2024.
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      Temporim, F. A., Bellon, U. D., Domeier, M., Trindade, R. I. F. da, D'Agrella Filho, M. S., & Tohver, E. (2021). Constraining the Cambrian drift of Gondwana with new paleomagnetic data from post-collisional plutons of the Araçuaí orogen, SE Brazil. Precambrian Research, 359, art. 106212. doi:10.1016/j.precamres.2021.106212
    • NLM

      Temporim FA, Bellon UD, Domeier M, Trindade RIF da, D'Agrella Filho MS, Tohver E. Constraining the Cambrian drift of Gondwana with new paleomagnetic data from post-collisional plutons of the Araçuaí orogen, SE Brazil [Internet]. Precambrian Research. 2021 ; 359 art. 106212.[citado 2024 jun. 13 ] Available from: https://doi.org/10.1016/j.precamres.2021.106212
    • Vancouver

      Temporim FA, Bellon UD, Domeier M, Trindade RIF da, D'Agrella Filho MS, Tohver E. Constraining the Cambrian drift of Gondwana with new paleomagnetic data from post-collisional plutons of the Araçuaí orogen, SE Brazil [Internet]. Precambrian Research. 2021 ; 359 art. 106212.[citado 2024 jun. 13 ] Available from: https://doi.org/10.1016/j.precamres.2021.106212
  • Source: Journal of Geophysical Research: Atmospheres. Unidade: IAG

    Subjects: INTERAÇÃO AR-MAR, TURBULÊNCIA ATMOSFÉRICA

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      HACKEROTT, João A et al. The role of roughness and stability on the momentum flux in the Marine Atmospheric Surface Layer: a study on the Southwestern Atlantic Ocean. Journal of Geophysical Research: Atmospheres, v. 123, n. 8, p. 3914-3932, 2018Tradução . . Disponível em: https://doi.org/10.1002/2017JD027994. Acesso em: 13 jun. 2024.
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      Hackerott, J. A., Pezzi, L. P., Bakhoday Paskyabi, M., Oliveira, A. P. de, Reuder, J., Souza, R. B. de, & Camargo, R. de. (2018). The role of roughness and stability on the momentum flux in the Marine Atmospheric Surface Layer: a study on the Southwestern Atlantic Ocean. Journal of Geophysical Research: Atmospheres, 123( 8), 3914-3932. doi:10.1002/2017JD027994
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      Hackerott JA, Pezzi LP, Bakhoday Paskyabi M, Oliveira AP de, Reuder J, Souza RB de, Camargo R de. The role of roughness and stability on the momentum flux in the Marine Atmospheric Surface Layer: a study on the Southwestern Atlantic Ocean [Internet]. Journal of Geophysical Research: Atmospheres. 2018 ; 123( 8): 3914-3932.[citado 2024 jun. 13 ] Available from: https://doi.org/10.1002/2017JD027994
    • Vancouver

      Hackerott JA, Pezzi LP, Bakhoday Paskyabi M, Oliveira AP de, Reuder J, Souza RB de, Camargo R de. The role of roughness and stability on the momentum flux in the Marine Atmospheric Surface Layer: a study on the Southwestern Atlantic Ocean [Internet]. Journal of Geophysical Research: Atmospheres. 2018 ; 123( 8): 3914-3932.[citado 2024 jun. 13 ] Available from: https://doi.org/10.1002/2017JD027994
  • Source: Journal of Volcanology and Geothermal Research. Unidade: IAG

    Subjects: ESTRATIGRAFIA, PETROGRAFIA, GEOQUÍMICA

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      DE MIN, Angelo et al. Insights into the petrogenesis of low- and high-Ti basalts: stratigraphy and geochemistry of four lava sequences from the central Paraná basin. Journal of Volcanology and Geothermal Research, v. 355, p. 232-252, 2018Tradução . . Disponível em: https://doi.org/10.1016/j.jvolgeores.2017.08.009. Acesso em: 13 jun. 2024.
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      De Min, A., Callegaro, S., Marzoli, A., Nardy, A. J. R., Chiaradia, M., Marques, L. S., & Gabbarrini, I. (2018). Insights into the petrogenesis of low- and high-Ti basalts: stratigraphy and geochemistry of four lava sequences from the central Paraná basin. Journal of Volcanology and Geothermal Research, 355, 232-252. doi:10.1016/j.jvolgeores.2017.08.009
    • NLM

      De Min A, Callegaro S, Marzoli A, Nardy AJR, Chiaradia M, Marques LS, Gabbarrini I. Insights into the petrogenesis of low- and high-Ti basalts: stratigraphy and geochemistry of four lava sequences from the central Paraná basin [Internet]. Journal of Volcanology and Geothermal Research. 2018 ; 355 232-252.[citado 2024 jun. 13 ] Available from: https://doi.org/10.1016/j.jvolgeores.2017.08.009
    • Vancouver

      De Min A, Callegaro S, Marzoli A, Nardy AJR, Chiaradia M, Marques LS, Gabbarrini I. Insights into the petrogenesis of low- and high-Ti basalts: stratigraphy and geochemistry of four lava sequences from the central Paraná basin [Internet]. Journal of Volcanology and Geothermal Research. 2018 ; 355 232-252.[citado 2024 jun. 13 ] Available from: https://doi.org/10.1016/j.jvolgeores.2017.08.009
  • Source: Boundary-Layer Meteorology. Unidade: IAG

    Subjects: MICROMETEOROLOGIA, TEMPERATURA, INTERAÇÃO BIOSFERA-ATMOSFERA

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      HACKEROTT, João A et al. A Surface-Layer Study of the Transport and Dissipation of Turbulent Kinetic Energy and the Variances of Temperature, Humidity and CO2. Boundary-Layer Meteorology, v. 165, n. 2, p. 211-231, 2017Tradução . . Disponível em: https://doi.org/10.1007/s10546-017-0271-0. Acesso em: 13 jun. 2024.
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      Hackerott, J. A., Paskyabi, M. B., Reuder, J., Oliveira, A. P. de, Kral, S. T., Marques Filho, E. P., et al. (2017). A Surface-Layer Study of the Transport and Dissipation of Turbulent Kinetic Energy and the Variances of Temperature, Humidity and CO2. Boundary-Layer Meteorology, 165( 2), 211-231. doi:10.1007/s10546-017-0271-0
    • NLM

      Hackerott JA, Paskyabi MB, Reuder J, Oliveira AP de, Kral ST, Marques Filho EP, Mesquita M dos S, Camargo R de. A Surface-Layer Study of the Transport and Dissipation of Turbulent Kinetic Energy and the Variances of Temperature, Humidity and CO2 [Internet]. Boundary-Layer Meteorology. 2017 ; 165( 2): 211-231.[citado 2024 jun. 13 ] Available from: https://doi.org/10.1007/s10546-017-0271-0
    • Vancouver

      Hackerott JA, Paskyabi MB, Reuder J, Oliveira AP de, Kral ST, Marques Filho EP, Mesquita M dos S, Camargo R de. A Surface-Layer Study of the Transport and Dissipation of Turbulent Kinetic Energy and the Variances of Temperature, Humidity and CO2 [Internet]. Boundary-Layer Meteorology. 2017 ; 165( 2): 211-231.[citado 2024 jun. 13 ] Available from: https://doi.org/10.1007/s10546-017-0271-0

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