Holocene sea level changes in the tierra del fuego region

Holocene sea level changes in the tierra del fuego region

dc.creatorMörner, N. A.
dc.date1991-06-01
dc.date.accessioned2022-12-15T19:38:33Z
dc.date.available2022-12-15T19:38:33Z
dc.identifierhttps://ppegeo.igc.usp.br/index.php/bigsp/article/view/2967
dc.identifier10.11606/issn.2317-8078.v0i8p133-151
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/5358124
dc.descriptionAvailable sea level data from the Tierra del Fuego region cannot be combined Into a meaningful sea level graph as recently proposed (PORTER et al., 1984 and RABASSA et al., 1986) because these records are dominated by sites of local seismotectonic uplift; i.e., the exceptions, not the rule. The general sea level tendency (i.e., the rule), gives a sea level rise from 9,000 up to about 4,000 BP when the peak-level was reached. This Holocene maximum level was, however, at or Just above the present sea level; ranging from zero via 0.5-1.0 m up to 1-2 m above the present sea level. A preliminary regional eustatic curve is proposed. Presently available sea level data do not record any Holocene glacial Isostatic effects.en-US
dc.formatapplication/pdf
dc.languageeng
dc.publisherUniversidade de São Paulo, Instituto de Geociênciaspt-BR
dc.relationhttps://ppegeo.igc.usp.br/index.php/bigsp/article/view/2967/2520
dc.rightsDireitos autorais 2016 Boletim IG-USP. Publicação Especialpt-BR
dc.sourceBoletim IG-USP. Publicação Especial; n. 8 (1991): Proceedings of the Global Changes in South America during the Quaternary; 133-151pt-BR
dc.source2317-8078
dc.source0102-6275
dc.titleHolocene sea level changes in the tierra del fuego regionen-US
dc.titleHolocene sea level changes in the tierra del fuego regionpt-BR
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typept-BR


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