scholarly journals SYN-COLLISIONAL PERALUMINOUS MAGMATISM IN THE RIO DOCE REGION: MINERALOGY, GEOCHEMISTRY AND ISOTOPIC DATA OF THE NEOPROTEROZOIC URUCUM SUITE (EASTERN MINAS GERAIS STATE, BRAZIL)

2000 ◽  
Vol 30 (1) ◽  
pp. 120-125 ◽  
Author(s):  
HERMÍNIO ARIAS NALINI JR ◽  
ESSAID BILAL ◽  
JOSÉ MARQUES CORREIA NEVES
2006 ◽  
Vol 78 (3) ◽  
pp. 543-556 ◽  
Author(s):  
Ciro A. Ávila ◽  
Wilson Teixeira ◽  
Umberto G. Cordani ◽  
Héctor R. Barrueto ◽  
Ronaldo M. Pereira ◽  
...  

The Glória quartz-monzodiorite, one of the mafic plutons of the Paleoproterozoic Mineiro belt, is intrusive into banded gneisses, amphibolites, schists and phyllites of the Rio das Mortes greenstone belt, in the southern portion of the São Francisco Craton, State of Minas Gerais, Brazil. The Glória quartz-monzodiorite yields a SHRIMP U-Pb zircon age of 2188 ± 29 Ma, suggesting a tectonic relationship with the pre-collisional phase of the Mineiro belt. According to the Nd isotopic evidence (epsilonNd(T) = -3.4; T DM = 2.68 Ga) the original magmas was formed by a mixture among Archean crustal material and Paleoproterozoic juvenile magma. The Glória quartz-monzodiorite shows metaluminous and calc-alkaline tendency with intermediate K content, comparable to that of volcanic-arc rocks. The primary mineralogical assemblage was partly modified by metamorphism, dated between 2131-2121 Ma in nearby coeval plutons. Such metamorphism is significantly older than the reported metamorphic episodes of the Mineiro belt in the Quadrilátero Ferrífero region (2059-2041 Ma) in the eastern portion of the study area. This evidence, together with chemical and isotopic data from other mafic and felsic plutons coeval with the Glória quartz-monzodiorite, indicate a tectonic and magmatic migration within the Mineiro belt from west to east.


Author(s):  
Ricardo Dalagnol ◽  
Carolina B. Gramcianinov ◽  
Natália Machado Crespo ◽  
Rafael Luiz ◽  
Julio Barboza Chiquetto ◽  
...  

2021 ◽  
Vol 108 ◽  
pp. 103349
Author(s):  
David Oldack Barcelos Ferreira Machado ◽  
Karina Ferreira Chueng ◽  
Heloisa Helena Gomes Coe ◽  
Alexandre Christófaro Silva ◽  
Camila Rodrigues Costa

2013 ◽  
Vol 71 (9) ◽  
pp. 4177-4186 ◽  
Author(s):  
Aline Sueli de Lima Rodrigues ◽  
Guilherme Malafaia ◽  
Adivane Terezinha Costa ◽  
Hermínio Arias Nalini Júnior

Author(s):  
Bruno Montijo Silva ◽  
Willian Cristof Correia Queiroz ◽  
Maerle Oliveira Maia ◽  
Richard de Campos Pacheco ◽  
Daniel Moura Aguiar ◽  
...  

2012 ◽  
Vol 111 (5) ◽  
pp. 1913-1921 ◽  
Author(s):  
Jörg Heukelbach ◽  
Raphael Frank ◽  
Liana Ariza ◽  
Íris de Sousa Lopes ◽  
Alcides de Assis e Silva ◽  
...  

Author(s):  
Edvânia Beatriz dos Santos PEREIRA ◽  
Sâmara Lauren Cunha RODRIGUES ◽  
Gustavo Henrique BAHIA-DE-OLIVEIRA ◽  
Suedali Villas Bôas COELHO ◽  
Ricardo Andrade BARATA

2010 ◽  
Vol 52 (4) ◽  
pp. 207-210 ◽  
Author(s):  
Hudson Alves Pinto ◽  
Alan Lane de Melo

Pleurolophocercous cercariae emerged from naturally infected Melanoides tuberculata from Minas Gerais State, Brazil, were used to perform experimental infection of laboratory-reared Poecilia reticulata. Mature metacercariae were obtained from the gills of fishes and force-fed to Mus musculus. The adult parasites which recovered from small intestines of mice were identified as Centrocestus formosanus. This is the first report of M. tuberculata as intermediate host of this heterophyid in Brazil.


Zootaxa ◽  
2021 ◽  
Vol 4958 (1) ◽  
pp. 160-166
Author(s):  
OSÉIAS MARTINS MAGALHÃES ◽  
GUSTAVO LISBOA VIEIRA MACHADO ◽  
MARCO ANTONIO ALVES CARNEIRO ◽  
FELIPE FERRAZ FIGUEIREDO MOREIRA

Microvelia joceliae Magalhães & Moreira, sp. nov. is described and illustrated based on material from Parque Natural Municipal das Andorinhas, Minas Gerais State, in southeastern Brazil. The new species can be distinguished from congeners occurring in the region by the pronotum of the apterous form covering almost the entire thorax dorsally, proepisternum with black denticles, male abdominal segments V–VII ventrally depressed, shape of the asymmetrical parameres, and female abdominal laterotergites reflected over the mediotergites and almost touching over segments V–VII. 


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