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Geochemistry of the Lower Protezoroic Granulite-Facies Grant Syenite Gneiss, Barra Velha, Santa Catarina State, Southern Brazil.
(Instituto de Geociências /Universidade Federal do Rio Grande do Sul, 1998)
METAMORPHIC CONDITIONS IN THE SANTA MARIA CHICO GRANULITE COMPLEX, RSCONDIÇÕES DE METAMORFISMO NO COMPLEXO GRANULÍTICO SANTA MARIA CHICO, RS
(Sociedade Brasileira de Geologia, 2017)
Metamorphic P-T evolution of granulites in the central Ribeira Fold Belt, SE Brazil
(SPRINGER HEIDELBERG, 2011)
Pseudosections, geothermobarometric estimates and careful petrographic observations of gneissic migmatites and granulites from Neoproterozoic central Ribeira Fold Belt (SE Brazil) were performed in order to quantify the ...
Granulitos da Região da Várzea do Capivarita Bloco Encruzilhada do Sul, RS
(Instituto de Geociências /Universidade Federal do Rio Grande do Sul, 1998)
Sulfur and carbon isotopes in scapolite-bearing granulites of the São José do Rio Pardo area, Brazil
(1992-07-01)
Sulfur and carbon isotope compositions of ten scapolites from granulite-facies rocks of the São José do Rio Pardo area, Guaxupé Complex, Brazil, were measured. Scapolite is the primary and major rock-forming mineral in ...
Sulfur and carbon isotopes in scapolite-bearing granulites of the São José do Rio Pardo area, Brazil
(1992-07-01)
Sulfur and carbon isotope compositions of ten scapolites from granulite-facies rocks of the São José do Rio Pardo area, Guaxupé Complex, Brazil, were measured. Scapolite is the primary and major rock-forming mineral in ...
Metamorphic evolution of the Sierras de San Luis, Argentina: granulite facies metamorphism related to mafic intrusions
(Springer Wien, 2001-01)
The Sierras de San Luis, which are part of the Sierras Pampeanas, are located in Central Argentina. The crystalline basement of the Sierras de San Luis is built up of three main blocks (western block, central block, and ...
Granulite-facies metamorphism at ca. 570-580 Ma in the Porangatu Granulite Complex, central Brazil: implications for the evolution of the Transbrasiliano LineamentMetamorfismo da fácies granulito em 570-580 Ma no Complexo Granulítico Porangatu, centro do Brasil: implicações para a evolução do Lineamento Transbrasiliano
(Sociedade Brasileira de Geologia, 2017)