Source: Communications Earth & Environment. Unidade: IGC
Subjects: GEOCRONOLOGIA, MAGMA, MAGMATISMO
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: 06 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. 06 ] 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. 06 ] Available from: https://doi.org/10.1038/s43247-021-00103-z