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Please use this identifier to cite or link to this item: http://acervodigital.unesp.br/handle/11449/64535
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dc.contributor.authorPerinotto, José Alexandre de Jesus-
dc.contributor.authorBonotto, Daniel Marcos-
dc.date.accessioned2014-05-27T11:17:58Z-
dc.date.accessioned2016-10-25T18:13:24Z-
dc.date.available2014-05-27T11:17:58Z-
dc.date.available2016-10-25T18:13:24Z-
dc.date.issued1994-12-01-
dc.identifier.citationGeociencias (Sao Paulo), v. 13, n. 2, p. 359-369, 1994.-
dc.identifier.urihttp://hdl.handle.net/11449/64535-
dc.identifier.urihttp://acervodigital.unesp.br/handle/11449/64535-
dc.description.abstractDuring a basinal scale study on Palermo Formation (Upper Permian, Parana Basin) high elevated Gamma Ray picks were identified mainly in the lower third of that stratigraphic unit. Those Gamma Ray signatures have been used as good regional stratigraphic markers. From them it was possible one chronostratigraphic analysis of Palermo Formation as pointed out by previous papers (Perinotto). Potassium40 is the responsible for the high Gamma Ray picks in the Palermo Formation. -from English summaryen
dc.format.extent359-369-
dc.language.isopor-
dc.sourceScopus-
dc.subjectchronostratigraphy-
dc.subjectgamma ray anomaly-
dc.subjectPermian-
dc.subjectpotassium-40-
dc.subjectstratigraphy-
dc.subjectBrazil, Parana Basin-
dc.titleMarcos estratigraficos regionais na Formacao Palermo: caracterizacao dos picos radioativospt
dc.title.alternativeRegional stratigraphic benchmarks in the Palermo Formation: characterization of radioactivity peaksen
dc.typeoutro-
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)-
dc.rights.accessRightsAcesso restrito-
dc.relation.ispartofGeociencias (Sao Paulo)-
dc.identifier.scopus2-s2.0-0028594335-
Appears in Collections:Artigos, TCCs, Teses e Dissertações da Unesp

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