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Artigo de periodico
How long can the middle crust remain partially molten during orogeny? (2018)
Cavalcante, Carolina ; Hollanda, Maria Helena Bezerra Maia de ; Vauchez, Alain ; Kawata, Marcelo Takei
Source: Geology. Unidade: IGC
Subjects: OROGÊNESE, GEOCRONOLOGIA
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
CAVALCANTE, Carolina et al. How long can the middle crust remain partially molten during orogeny?. Geology, v. 46, n. 10, p. 839-842, 2018Tradução . . Disponível em: https://doi.org/10.1130/g45126.1. Acesso em: 08 nov. 2024.
APA
Cavalcante, C., Hollanda, M. H. B. M. de, Vauchez, A., & Kawata, M. T. (2018). How long can the middle crust remain partially molten during orogeny? Geology, 46( 10), 839-842. doi:10.1130/g45126.1
NLM
Cavalcante C, Hollanda MHBM de, Vauchez A, Kawata MT. How long can the middle crust remain partially molten during orogeny? [Internet]. Geology. 2018 ; 46( 10): 839-842.[citado 2024 nov. 08 ] Available from: https://doi.org/10.1130/g45126.1
Vancouver
Cavalcante C, Hollanda MHBM de, Vauchez A, Kawata MT. How long can the middle crust remain partially molten during orogeny? [Internet]. Geology. 2018 ; 46( 10): 839-842.[citado 2024 nov. 08 ] Available from: https://doi.org/10.1130/g45126.1
Artigo de periodico
Self-indentation of a heterogeneous continental lithosphere (1994)
Vauchez, Alain ; Tommasi, Andrea ; Egydio-Silva, Marcos
Source: Geology. Unidade: IGC
Assunto: GEOLOGIA ESTRUTURAL
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
VAUCHEZ, Alain e TOMMASI, Andrea e EGYDIO-SILVA, Marcos. Self-indentation of a heterogeneous continental lithosphere. Geology, v. 22, n. 11, p. 967-70, 1994Tradução . . Disponível em: https://doi.org/10.1130/0091-7613(1994)022<0967:sioahc>2.3.co;2. Acesso em: 08 nov. 2024.
APA
Vauchez, A., Tommasi, A., & Egydio-Silva, M. (1994). Self-indentation of a heterogeneous continental lithosphere. Geology, 22( 11), 967-70. doi:10.1130/0091-7613(1994)022<0967:sioahc>2.3.co;2
NLM
Vauchez A, Tommasi A, Egydio-Silva M. Self-indentation of a heterogeneous continental lithosphere [Internet]. Geology. 1994 ; 22( 11): 967-70.[citado 2024 nov. 08 ] Available from: https://doi.org/10.1130/0091-7613(1994)022<0967:sioahc>2.3.co;2
Vancouver
Vauchez A, Tommasi A, Egydio-Silva M. Self-indentation of a heterogeneous continental lithosphere [Internet]. Geology. 1994 ; 22( 11): 967-70.[citado 2024 nov. 08 ] Available from: https://doi.org/10.1130/0091-7613(1994)022<0967:sioahc>2.3.co;2
Artigo de periodico
Termination of a continental scale strike-slip fault in partially melted crust: the west Pernambuco shear zone, northeast Brazil (1992)
Vauchez, Alain ; Egydio-Silva, Marcos
Source: Geology. Unidade: IGC
Subjects: GEOLOGIA ESTRUTURAL, GEOTECTÔNICA
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
VAUCHEZ, Alain e EGYDIO-SILVA, Marcos. Termination of a continental scale strike-slip fault in partially melted crust: the west Pernambuco shear zone, northeast Brazil. Geology, v. 20, n. 11, p. 1007-10, 1992Tradução . . Disponível em: https://doi.org/10.1130/0091-7613(1992)020<1007:TOACSS>2.3.CO;2. Acesso em: 08 nov. 2024.
APA
Vauchez, A., & Egydio-Silva, M. (1992). Termination of a continental scale strike-slip fault in partially melted crust: the west Pernambuco shear zone, northeast Brazil. Geology, 20( 11), 1007-10. doi:10.1130/0091-7613(1992)020<1007:TOACSS>2.3.CO;2
NLM
Vauchez A, Egydio-Silva M. Termination of a continental scale strike-slip fault in partially melted crust: the west Pernambuco shear zone, northeast Brazil [Internet]. Geology. 1992 ; 20( 11): 1007-10.[citado 2024 nov. 08 ] Available from: https://doi.org/10.1130/0091-7613(1992)020<1007:TOACSS>2.3.CO;2
Vancouver
Vauchez A, Egydio-Silva M. Termination of a continental scale strike-slip fault in partially melted crust: the west Pernambuco shear zone, northeast Brazil [Internet]. Geology. 1992 ; 20( 11): 1007-10.[citado 2024 nov. 08 ] Available from: https://doi.org/10.1130/0091-7613(1992)020<1007:TOACSS>2.3.CO;2

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