Ganade, Carlos E. 
; Lanari, Pierre ; Rubatto, Daniela ; Hermann, Joerg ; Weinberg, Roberto F. ; Basei, Miguel Angelo Stipp ; Tesser, Lucas R. ; Caby, Renaud ; Agbossoumounde, Yao; Ribeiro, Caroline M.
Fonte: Communications Earth & Environment. Unidade: IGC
Assuntos: GEOCRONOLOGIA, MAGMA, MAGMATISMO
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ABNT
GANADE, Carlos E. et al. Magmatic flare-up causes crustal thickening at the transition from subduction to continental collision. Communications Earth & Environment, v. 2, n. 41, p. -, 2021Tradução . . Disponível em: https://doi.org/10.1038/s43247-021-00103-z. Acesso em: 12 nov. 2024.APA
Ganade, C. E., Lanari, P., Rubatto, D., Hermann, J., Weinberg, R. F., Basei, M. A. S., et al. (2021). Magmatic flare-up causes crustal thickening at the transition from subduction to continental collision. Communications Earth & Environment, 2( 41), -. doi:10.1038/s43247-021-00103-zNLM
Ganade CE, Lanari P, Rubatto D, Hermann J, Weinberg RF, Basei MAS, Tesser LR, Caby R, Agbossoumounde Y, Ribeiro CM. Magmatic flare-up causes crustal thickening at the transition from subduction to continental collision [Internet]. Communications Earth & Environment. 2021 ; 2( 41): -.[citado 2024 nov. 12 ] Available from: https://doi.org/10.1038/s43247-021-00103-zVancouver
Ganade CE, Lanari P, Rubatto D, Hermann J, Weinberg RF, Basei MAS, Tesser LR, Caby R, Agbossoumounde Y, Ribeiro CM. Magmatic flare-up causes crustal thickening at the transition from subduction to continental collision [Internet]. Communications Earth & Environment. 2021 ; 2( 41): -.[citado 2024 nov. 12 ] Available from: https://doi.org/10.1038/s43247-021-00103-z
