Seismostratigraphy of the Ceará Plateau: clues to decipher the Cenozoic evolution of Brazilian Equatorial Margin (2016)
- Authors:
- USP affiliated authors: JOVANE, LUIGI - IO ; MOLINA, EDER CASSOLA - IAG
- Unidades: IO; IAG
- DOI: 10.3389/feart.2016.00090
- Subjects: SISMOESTRATIGRAFIA; CENOZOICO; BACIAS SEDIMENTARES
- Language: Inglês
- Imprenta:
- Source:
- Título: Frontiers in Earth Sciences
- ISSN: 2296-701X
- Volume/Número/Paginação/Ano: v. 4, p. 90/1-90/14, 2016
- Este periódico é de acesso aberto
- Este artigo NÃO é de acesso aberto
-
ABNT
JOVANE, Luigi et al. Seismostratigraphy of the Ceará Plateau: clues to decipher the Cenozoic evolution of Brazilian Equatorial Margin. Frontiers in Earth Sciences, v. 4, p. 90/1-90/14, 2016Tradução . . Disponível em: https://doi.org/10.3389/feart.2016.00090. Acesso em: 21 jan. 2026. -
APA
Jovane, L., Figueiredo, J. J. P., Alves, D. P. V., Lacopini, D., & Molina, E. C. (2016). Seismostratigraphy of the Ceará Plateau: clues to decipher the Cenozoic evolution of Brazilian Equatorial Margin. Frontiers in Earth Sciences, 4, 90/1-90/14. doi:10.3389/feart.2016.00090 -
NLM
Jovane L, Figueiredo JJP, Alves DPV, Lacopini D, Molina EC. Seismostratigraphy of the Ceará Plateau: clues to decipher the Cenozoic evolution of Brazilian Equatorial Margin [Internet]. Frontiers in Earth Sciences. 2016 ; 4 90/1-90/14.[citado 2026 jan. 21 ] Available from: https://doi.org/10.3389/feart.2016.00090 -
Vancouver
Jovane L, Figueiredo JJP, Alves DPV, Lacopini D, Molina EC. Seismostratigraphy of the Ceará Plateau: clues to decipher the Cenozoic evolution of Brazilian Equatorial Margin [Internet]. Frontiers in Earth Sciences. 2016 ; 4 90/1-90/14.[citado 2026 jan. 21 ] Available from: https://doi.org/10.3389/feart.2016.00090 - Sismostratigraphy of the Ceará Plateau to decipher the cenozoic evolution of Brazilian Equatorial Margin
- Gravity and Magnetic Constraints on the Crustal Structure of the Ceará Plateau, Brazilian Equatorial Margin
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Informações sobre o DOI: 10.3389/feart.2016.00090 (Fonte: oaDOI API)
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