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Please use this identifier to cite or link to this item: http://acervodigital.unesp.br/handle/11449/64095
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dc.contributor.authorWernick, E.-
dc.contributor.authorFerreira, C. J.-
dc.date.accessioned2014-05-27T11:17:24Z-
dc.date.accessioned2016-10-25T18:12:40Z-
dc.date.available2014-05-27T11:17:24Z-
dc.date.available2016-10-25T18:12:40Z-
dc.date.issued1990-12-01-
dc.identifier.citationGeociencias, v. 9, p. 107-125.-
dc.identifier.issn0101-9082-
dc.identifier.urihttp://hdl.handle.net/11449/64095-
dc.identifier.urihttp://acervodigital.unesp.br/handle/11449/64095-
dc.description.abstractSr87/86Sr initial ratio data based on the isochrons from 22 granitoid complexes of Brasiliano age (Late Precambrian) from S and E Brazil are presented. The complexes have been classified into different rock series with the aid of zircon typology. A correlation between the initial ratio and the zircon typology can be determined. Of particular interest is the systematic decrease of the Sr87/86Sr initial ratio in the range from the low, through medium to the high temperature calc-alkaline series which could indicate a gradual increasing of mantle material in the genesis of calc-alkaline granitoid of progressive greater depths. -from English summaryen
dc.format.extent107-125-
dc.language.isopor-
dc.sourceScopus-
dc.subjectBrasiliano-
dc.subjectcalc-alkaline rock-
dc.subjectgranite-
dc.subjectisotopic analysis-
dc.subjectmantle material-
dc.subjectstrontium-
dc.subjectzircon-
dc.subjectBrazil-
dc.titleTipologia de zircao e razao inicial Sr87/86Sr em series granitoidespt
dc.title.alternativeZircon typology and Sr87/Sr86 ratio in granitoid seriesen
dc.typeoutro-
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)-
dc.rights.accessRightsAcesso restrito-
dc.relation.ispartofGeociências-
dc.identifier.scopus2-s2.0-0025683413-
Appears in Collections:Artigos, TCCs, Teses e Dissertações da Unesp

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