Geochemistry of the Guaxupe Granulites, Minas Gerais, Brazil


Autoria(s): Del Lama, E. A.; de Oliveira, MAF; Zanardo, A.
Contribuinte(s)

Universidade Estadual Paulista (UNESP)

Data(s)

20/05/2014

20/05/2014

01/10/1998

Resumo

Geochemical 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.

Formato

357-365

Identificador

http://dx.doi.org/10.1016/S1342-937X(05)70851-0

Gondwana Research. Osaka: Int Associação Gondwana Research, v. 1, n. 3-4, p. 357-365, 1998.

1342-937X

http://hdl.handle.net/11449/37649

10.1016/S1342-937X(05)70851-0

WOS:000080990700007

Idioma(s)

eng

Publicador

Int Associação Gondwana Research

Relação

Gondwana Research

Direitos

closedAccess

Palavras-Chave #granulites #REE #lower crust #Guaxupe Massif #Brazil
Tipo

info:eu-repo/semantics/article