Evidence of late quaternary sealevel stillstands on the upper brazilian continental margin: a synthesis

KOWSMANN, Renato Oscar; COSTA, Márcio Paulo de Ataíde

Use este identificador para citar ou linkar para este item: https://rigeo.sgb.gov.br/handle/doc/24685

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Campo DC	Valor	Idioma
dc.contributor.author	KOWSMANN, Renato Oscar	-
dc.contributor.author	COSTA, Márcio Paulo de Ataíde	-
dc.date.accessioned	2024-01-29T18:53:21Z	-
dc.date.available	2024-01-29T18:53:21Z	-
dc.date.issued	1979	-
dc.identifier.citation	KOWSMANN, 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.uri	https://rigeo.sgb.gov.br/handle/doc/24685	-
dc.description.abstract	Notable 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.iso	en	pt_BR
dc.publisher	[s. n.]	pt_BR
dc.rights	open	pt_BR
dc.subject	MARGEM CONTINENTAL BRASILEIRA	-
dc.subject	BATIMETRIA	-
dc.title	Evidence of late quaternary sealevel stillstands on the upper brazilian continental margin: a synthesis	pt_BR
dc.type	Working Paper	pt_BR
dc.local	São Paulo	pt_BR
dc.subject.en	BRAZILIAN CONTINENTAL MARGIN	pt_BR
dc.subject.en	BATHYMETRY	pt_BR
dc.subject.en	SURFACE SEDIMENTS	pt_BR
dc.subject.en	SEA LEVEL	pt_BR
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