Geochemistry of the Guaxupe Granulites, Minas Gerais, Brazil

dc.contributorUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2014-05-20T15:27:43Z
dc.date.accessioned2022-10-05T16:44:54Z
dc.date.available2014-05-20T15:27:43Z
dc.date.available2022-10-05T16:44:54Z
dc.date.created2014-05-20T15:27:43Z
dc.date.issued1998-10-01
dc.identifierGondwana Research. Osaka: Int Associação Gondwana Research, v. 1, n. 3-4, p. 357-365, 1998.
dc.identifier1342-937X
dc.identifierhttp://hdl.handle.net/11449/37649
dc.identifier10.1016/S1342-937X(05)70851-0
dc.identifierWOS:000080990700007
dc.identifier6893272900174059
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/3909132
dc.description.abstractGeochemical data for granulite terrain are presented from the northernmost portion of the Guaxupe Massif, at Mantiqueira Province, SE Brazil. Several types of granulites are recognized in the area: basic, intermediate and acid granulite. Major and trace elements (including REE) point to only one ma,oma source for these granulites generated at different times. Geochemical data point to plagioclase and apatite fractionation as responsable in the REE behaviour in intermediate and more basic rocks. Overall composition of the Guaxupe Granulites is similar to average composition of the lower crust.
dc.languageeng
dc.publisherInt Associação Gondwana Research
dc.relationGondwana Research
dc.relation5.657
dc.rightsAcesso restrito
dc.sourceWeb of Science
dc.subjectgranulites
dc.subjectREE
dc.subjectlower crust
dc.subjectGuaxupe Massif
dc.subjectBrazil
dc.titleGeochemistry of the Guaxupe Granulites, Minas Gerais, Brazil
dc.typeArtigo


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