Cavalcante, Carolina 
; Vauchez, Alain ; Egydio-Silva, Marcos ; Hollanda, Maria Helena Bezerra Maia de ; Boyer, B.
Fonte: Solid Earth. Unidade: IGC
Assuntos: GEOLOGIA ESTRUTURAL, OROGÊNESE, CROSTA DA TERRA
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CAVALCANTE, Carolina et al. Thermal conditions during deformation of partially molten crust from TitaniQ geothermometry: rheological implications for the anatectic domain of the Araçuaí belt, eastern Brazil. Solid Earth, v. 5, n. 2, p. 1223-1242, 2014Tradução . . Disponível em: https://doi.org/10.5194/se-5-1223-2014. Acesso em: 21 ago. 2024.APA
Cavalcante, C., Vauchez, A., Egydio-Silva, M., Hollanda, M. H. B. M. de, & Boyer, B. (2014). Thermal conditions during deformation of partially molten crust from TitaniQ geothermometry: rheological implications for the anatectic domain of the Araçuaí belt, eastern Brazil. Solid Earth, 5( 2), 1223-1242. doi:10.5194/se-5-1223-2014NLM
Cavalcante C, Vauchez A, Egydio-Silva M, Hollanda MHBM de, Boyer B. Thermal conditions during deformation of partially molten crust from TitaniQ geothermometry: rheological implications for the anatectic domain of the Araçuaí belt, eastern Brazil [Internet]. Solid Earth. 2014 ; 5( 2): 1223-1242.[citado 2024 ago. 21 ] Available from: https://doi.org/10.5194/se-5-1223-2014Vancouver
Cavalcante C, Vauchez A, Egydio-Silva M, Hollanda MHBM de, Boyer B. Thermal conditions during deformation of partially molten crust from TitaniQ geothermometry: rheological implications for the anatectic domain of the Araçuaí belt, eastern Brazil [Internet]. Solid Earth. 2014 ; 5( 2): 1223-1242.[citado 2024 ago. 21 ] Available from: https://doi.org/10.5194/se-5-1223-2014
