Unraveling the metamorphic conditions of an alpine-type orogen in NE-Brazil: constraints from P-T paths of zoned garnet in the Riacho do Pontal Belt, Borborema Province (2023)
- Authors:
- USP affiliated authors: BASEI, MIGUEL ANGELO STIPP - IGC ; CIOFFI, CAUE RODRIGUES - IGC ; TESSER, LUCAS RAMOS - IGC
- Unidade: IGC
- Subjects: METAMORFISMO; COLISÕES
- Agências de fomento:
- Language: Inglês
- Imprenta:
- Source:
- Título: Anais SBGq
- Volume/Número/Paginação/Ano: p. 177, 2023
- Conference titles: Congresso Brasileiro de Geoquímica
-
ABNT
TESSER, Lucas R. et al. Unraveling the metamorphic conditions of an alpine-type orogen in NE-Brazil: constraints from P-T paths of zoned garnet in the Riacho do Pontal Belt, Borborema Province. 2023, Anais.. Aracajú: Instituto de Geociências, Universidade de São Paulo, 2023. p. 177. Disponível em: https://repositorio.usp.br/directbitstream/7b235414-f22d-4492-b901-641b868550a2/3151405.pdf. Acesso em: 30 dez. 2025. -
APA
Tesser, L. R., Ganade, C. E., Basei, M. A. S., & Cioffi, C. R. (2023). Unraveling the metamorphic conditions of an alpine-type orogen in NE-Brazil: constraints from P-T paths of zoned garnet in the Riacho do Pontal Belt, Borborema Province. In Anais SBGq (p. 177). Aracajú: Instituto de Geociências, Universidade de São Paulo. Recuperado de https://repositorio.usp.br/directbitstream/7b235414-f22d-4492-b901-641b868550a2/3151405.pdf -
NLM
Tesser LR, Ganade CE, Basei MAS, Cioffi CR. Unraveling the metamorphic conditions of an alpine-type orogen in NE-Brazil: constraints from P-T paths of zoned garnet in the Riacho do Pontal Belt, Borborema Province [Internet]. Anais SBGq. 2023 ; 177.[citado 2025 dez. 30 ] Available from: https://repositorio.usp.br/directbitstream/7b235414-f22d-4492-b901-641b868550a2/3151405.pdf -
Vancouver
Tesser LR, Ganade CE, Basei MAS, Cioffi CR. Unraveling the metamorphic conditions of an alpine-type orogen in NE-Brazil: constraints from P-T paths of zoned garnet in the Riacho do Pontal Belt, Borborema Province [Internet]. Anais SBGq. 2023 ; 177.[citado 2025 dez. 30 ] Available from: https://repositorio.usp.br/directbitstream/7b235414-f22d-4492-b901-641b868550a2/3151405.pdf - Magmatic flare-up causes crustal thickening at the transition from subduction to continental collision
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