Assuntos: TERMODINÂMICA, FALHAS (GEOLOGIA ESTRUTURAL), CISALHAMENTO
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TAUFNER, Rhander et al. Microstructures reveal brittle and viscous flow during exhumation of the high-temperature lower oceanic crust from Site U1473A, Atlantis Bank, Southwest Indian Ridge (IODP Expedition 360). 2021, Anais.. [S.l.]: Instituto de Geociências, Universidade de São Paulo, 2021. Disponível em: https://doi.org/10.5194/egusphere-egu21-1905. Acesso em: 03 nov. 2024.APA
Taufner, R., Viegas, G., Faleiros, F. M., Castellan, P., & Silva, R. (2021). Microstructures reveal brittle and viscous flow during exhumation of the high-temperature lower oceanic crust from Site U1473A, Atlantis Bank, Southwest Indian Ridge (IODP Expedition 360). In . Instituto de Geociências, Universidade de São Paulo. doi:10.5194/egusphere-egu21-1905NLM
Taufner R, Viegas G, Faleiros FM, Castellan P, Silva R. Microstructures reveal brittle and viscous flow during exhumation of the high-temperature lower oceanic crust from Site U1473A, Atlantis Bank, Southwest Indian Ridge (IODP Expedition 360) [Internet]. 2021 ;[citado 2024 nov. 03 ] Available from: https://doi.org/10.5194/egusphere-egu21-1905Vancouver
Taufner R, Viegas G, Faleiros FM, Castellan P, Silva R. Microstructures reveal brittle and viscous flow during exhumation of the high-temperature lower oceanic crust from Site U1473A, Atlantis Bank, Southwest Indian Ridge (IODP Expedition 360) [Internet]. 2021 ;[citado 2024 nov. 03 ] Available from: https://doi.org/10.5194/egusphere-egu21-1905