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Filtros : "Dominguez, José Maria Landim" "França" Removido: "Unesco Reports in Marine Science" Limpar

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Artigo de periodico
Quaternary sea-level history and variation in dynamics along the central brazilian coast: consequences on coastal plain construction (1996)
Martin, Louis; Suguio, Kenitiro; Flexor, Jean-Marie; Dominguez, José Maria Landim ; Bittencourt, Abílio C. S. P.
Source: Anais da Academia Brasileira de Ciências. Unidade: IGC
Subjects: SEDIMENTOLOGIA, ESTRATIGRAFIA
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
MARTIN, Louis et al. Quaternary sea-level history and variation in dynamics along the central brazilian coast: consequences on coastal plain construction. Anais da Academia Brasileira de Ciências, v. 68, n. 3 , p. 303-54, 1996Tradução . . Disponível em: http://memoria.bn.br/DocReader/158119/33905. Acesso em: 18 nov. 2024.
APA
Martin, L., Suguio, K., Flexor, J. -M., Dominguez, J. M. L., & Bittencourt, A. C. S. P. (1996). Quaternary sea-level history and variation in dynamics along the central brazilian coast: consequences on coastal plain construction. Anais da Academia Brasileira de Ciências, 68( 3 ), 303-54. Recuperado de http://memoria.bn.br/DocReader/158119/33905
NLM
Martin L, Suguio K, Flexor J-M, Dominguez JML, Bittencourt ACSP. Quaternary sea-level history and variation in dynamics along the central brazilian coast: consequences on coastal plain construction [Internet]. Anais da Academia Brasileira de Ciências. 1996 ; 68( 3 ): 303-54.[citado 2024 nov. 18 ] Available from: http://memoria.bn.br/DocReader/158119/33905
Vancouver
Martin L, Suguio K, Flexor J-M, Dominguez JML, Bittencourt ACSP. Quaternary sea-level history and variation in dynamics along the central brazilian coast: consequences on coastal plain construction [Internet]. Anais da Academia Brasileira de Ciências. 1996 ; 68( 3 ): 303-54.[citado 2024 nov. 18 ] Available from: http://memoria.bn.br/DocReader/158119/33905
Trabalho de evento-resumo
Sea-level changes during the Quaternary along the central part of the Brazilian coast: consequence on sandy sedimentation (1995)
Martin, Louis; Suguio, Kenitiro; Flexor, Jean-Marie; Dominguez, José Maria Landim ; Bittencourt, Abílio Carlos da Silva Pinto
Source: Program and abstracts. Conference titles: Land-Ocean Interactions in the Coastal Zone. Scientific Meeting. Unidade: IGC
Subjects: QUATERNÁRIO, NÍVEL DO MAR, SEDIMENTOLOGIA MARINHA
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
MARTIN, Louis et al. Sea-level changes during the Quaternary along the central part of the Brazilian coast: consequence on sandy sedimentation. 1995, Anais.. [S.l.]: Instituto de Geociências, Universidade de São Paulo, 1995. p. 001-002. Disponível em: https://repositorio.usp.br/directbitstream/18de98d3-4c4e-46bf-a2a8-9f9b4c8dc390/3080521.pdf. Acesso em: 18 nov. 2024.
APA
Martin, L., Suguio, K., Flexor, J. -M., Dominguez, J. M. L., & Bittencourt, A. C. da S. P. (1995). Sea-level changes during the Quaternary along the central part of the Brazilian coast: consequence on sandy sedimentation. In Program and abstracts (p. 001-002). [S.l.]: Instituto de Geociências, Universidade de São Paulo. Recuperado de https://repositorio.usp.br/directbitstream/18de98d3-4c4e-46bf-a2a8-9f9b4c8dc390/3080521.pdf
NLM
Martin L, Suguio K, Flexor J-M, Dominguez JML, Bittencourt AC da SP. Sea-level changes during the Quaternary along the central part of the Brazilian coast: consequence on sandy sedimentation [Internet]. Program and abstracts. 1995 ; 001-002.[citado 2024 nov. 18 ] Available from: https://repositorio.usp.br/directbitstream/18de98d3-4c4e-46bf-a2a8-9f9b4c8dc390/3080521.pdf
Vancouver
Martin L, Suguio K, Flexor J-M, Dominguez JML, Bittencourt AC da SP. Sea-level changes during the Quaternary along the central part of the Brazilian coast: consequence on sandy sedimentation [Internet]. Program and abstracts. 1995 ; 001-002.[citado 2024 nov. 18 ] Available from: https://repositorio.usp.br/directbitstream/18de98d3-4c4e-46bf-a2a8-9f9b4c8dc390/3080521.pdf

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