Please use this identifier to cite or link to this item: https://rigeo.sgb.gov.br/handle/doc/24685
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dc.contributor.authorKOWSMANN, Renato Oscar-
dc.contributor.authorCOSTA, Márcio Paulo de Ataíde-
dc.date.accessioned2024-01-29T18:53:21Z-
dc.date.available2024-01-29T18:53:21Z-
dc.date.issued1979-
dc.identifier.citationKOWSMANN, Renato Oscar; COSTA, Márcio Paulo de Ataíde. Evidence of late quaternary sea level stillstands on the upper brazilian continental margin: a synthesis. In: INTERNATIONAL SYMPOSIUM ON COASTAL EVOLUTION IN THE QUATERNARY, 1978, São Paulo. Proceedings [...]. São Paulo: [s. n.], 1979. p. 170-192.pt_BR
dc.identifier.urihttps://rigeo.sgb.gov.br/handle/doc/24685-
dc.description.abstractNotable regional evidence of Holocene stillstands of sea level was gathered along the upper Brazilian continental margin, based on sedimentological, environmental and morphological data. Six persistent levels were detected approximately following the present 130, 110, 90, 75, 60 and 40 m isobaths. Radiocarbon dates and comparison with the MILLIMAN and EMERY (1968) eustatic curve assigned ages ranging from the late Wisconsin glacial maximum at 15,000 years B. P. for the deepest level to 9,000 years B. P. for the shallowest level.pt_BR
dc.language.isoenpt_BR
dc.publisher[s. n.]pt_BR
dc.rightsopenpt_BR
dc.subjectMARGEM CONTINENTAL BRASILEIRA-
dc.subjectBATIMETRIA-
dc.titleEvidence of late quaternary sealevel stillstands on the upper brazilian continental margin: a synthesispt_BR
dc.typeWorking Paperpt_BR
dc.localSão Paulopt_BR
dc.subject.enBRAZILIAN CONTINENTAL MARGINpt_BR
dc.subject.enBATHYMETRYpt_BR
dc.subject.enSURFACE SEDIMENTSpt_BR
dc.subject.enSEA LEVELpt_BR
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