Granites
Mostrando 25-36 de 80 artigos, teses e dissertações.
-
25. Estratigrafia e petrogênese das sequências vulcânicas paleoproterozóicas na região de São Félix do Xingu (PA), Província Mineral de Carajás / Stratigraphy and petrogenesis of the paleoproterozoic volcanic sequences in the São Félix do Xingu (PA) region, Carajás Mineral Province
Near the São Félix do Xingu city, centersouth portion of the Pará state, in the context of the Carajás Mineral Province, occur extensive Paleoproterozoic volcanoplutonism (1.88 1.87 Ga) exceptionally well-preserved and grouped in the Sobreiro and Santa Rosa formations. These suites are generically correlated to Uatumã Supergroup volcanoplutonism, a magm
Publicado em: 2009
-
26. Geochemistry and petrogenesis of post-collisional ultrapotassic syenites and granites from southernmost Brazil: the Piquiri Syenite Massif
O Maciço Sienítico Piquirí, situado no extremo sul do Brasil, é parte do magmatismo pós-colisional neoproterozóico relacionado ao Ciclo Brasiliano-Pan-Africano. O maciço tem em torno de 12 km de diâmetro e é composto de sienitos, granitos, rochas monzoníticas e lamprófiros. Diopsídio-flogopita, diopsídio-biotita-augita- anfibólio cálcico são
Anais da Academia Brasileira de Ciências. Publicado em: 2008-06
-
27. DiagnÃstico do setor de rochas ornamentais e de revestimento do Estado de Pernambuco
In this work the geologic considerations on the granites diggings for ornamental ends are presented, a profile of the Brazilian sector of ornamental rocks and a diagnosis of the productive chain of the State of Pernambuco, involving the mining (main deposits, methods of cultivate, technology of cut for the dismounting of blocks), sawing shops and marble shop
Publicado em: 2008
-
28. Estado da arte na alterabilidade de placas pÃtreas: estudo de casos na regiÃo litorÃnea do Recife â PE
The importance of ornamental rocks in architecture is historical; either to the internal areas or to the external ones. Thus, in this study, covering alterability and durability regarding with stony plates in located land external faÃades in the sea shore of Recife are discussed. The civil construction industry uses, in workmanship, the most varied types of
Publicado em: 2008
-
29. Geoquimica e cronologia de alojamento de granitos colisionais na Faixa Sergipana, Nordeste do Brasil / Geochemistry and emplacement chronology of collisional granites in the Sergipano belt, NE-Brazil
A Faixa Sergipana é uma das mais significantes faixas móveis neoproterozóicas do nordeste do Brasil, porque ela contém diversas estruturas e domínios litológicos que permitem que ela seja comparada a orógenos fanerozóicos como os Himalaias, por exemplo. A Faixa Sergipana foi formada durante a colisão entre o Cráton São Francisco-Congo e o Maciço
Publicado em: 2008
-
30. Geoquímica de rocha total, geocronologia de u-pb e geologia isotópica de sm-nd das rochas ortognáissicas e unidades litológicas associadas da região ipameri - Catalão (Goiás)
The part of the southern Brasília Belt, Tocantins Province, exposed in central Brazil, comprises metasedimentary rocks, metavolcano-sedimentary sequences, amphibolites and intrusive granites, and a large orthogneiss belt. These units are tectonically imbricated, and vary in metamorphic grade from lower greenschist to amphibolite facies, characterized by a 7
Publicado em: 2008
-
31. Caracterização geoquímica-isotópica e geocronologia do enxame de diques de Manaíra-Princesa Isabel (PB) - Província Borborema / Geochemical-isotopic characterization and geocronology of the dike swarm of Manaíra-Princesa Isabel region (PB) - Borborema Province
The Manaíra-Princesa Isabel dike swarm forms one of the most expressive Neoproterozoic alkaline magmatism of the Borborema Province (NE Brazil). It consists of about a hundred NE-trending bodies intrusive in Neoproterozoic porphyritic granites (Princesa Isabel and Tavares plutons) and orthogneisses and low grade metasediments of the Eoneoproterozoic Riacho
Publicado em: 2008
-
32. Características de campo, petrografia e litogeoquímica da Unidade Santo Aleixo em sua localidade-tipo / Field geology, petrography and lithogeochemistry of Santo Aleixo Unit in its type location
The Santo Aleixo Unit in its type-location is represented by homogenous gneiss and subordinated banded and inclused mafic-felsic-rich gneisses, all rocks separated by gradational contacts. Leucogranitic gneiss, migmatites, late-tectonic granite stocks and diabase dikes also occur in the studied area. The gneissic foliation dips to SE or NW with low to medium
Publicado em: 2008
-
33. Contribuição ao estudo dos métodos de ensaio na avaliação das reações álcali-agregado em concretos. / Contribution to the study of test methods in assessing alkali-aggregate reactions in concrete.
Many concrete structures have been suffering from alkali-aggregate reactions (AAR) since the last decades in Brazil and around the world. The reactions generate expansions that could compromise the strength of a concrete structure as well as its performance in service and its durability. Nowadays, it is completely possible to detect AAR in the field, but rep
Publicado em: 2008
-
34. Geology of the Camboriú Complex (SC) / Geologia do Complexo Camboriú (SC)
The anatectic origin evidenced by known macrostructures in migmatites of the Camboriú Complex is supported by petrographical, geochemical and isotopic data, with partial melting under compressional regimen being suggested by the large amount of leucosome bodies at low-pressure sites represented by interboudins and dilation surfaces. Despite the continental
Publicado em: 2008
-
35. Processos metalogenéticos em ambientes de arco magmático tipo andino, caso de estudo: mineralizações da região dos Andes Patagônicos setentrionais do Chile / Metallogenic processes in andean volcanic arc setting, study case: mineralizations in the Chilean North-Patagonion Andes
In the Patagonian Andes region between 41 and 44° S extensive and continuous plutonic rocks of the North-Patagonian Batholith north segment are exposed. During their evolution most of the granitic rocks were emplaced in metamorphic rocks and other parts were emplaced in Late Jurassic-Berriasan volcanic rocks, Early Cretaceous sedimentary and volcanic rocks,
Publicado em: 2008
-
36. The Serra da Graciosa A-type granites and syenites, southern Brazil. Part 1: regional setting and geological characterization
A região da Serra da Graciosa inclui importantes ocorrências de granitos e sienitos da Província Graciosa de Tipo-A (originalmente chamada de Suite Serra do Mar), Sul do Brasil. Com base em trabalho de campo, petrografia, e imagens de sensoriamento remoto, é feita a caracterização dos plútons da região. Cinco plútons independentes são reconhecidos.
Anais da Academia Brasileira de Ciências. Publicado em: 2007-09