Archean granitoid magmatism in the Canaã dos Carajás area: Implications for crustal evolution of the Carajás province, Amazonian craton, Brazil

2013 ◽  
Vol 227 ◽  
pp. 157-185 ◽  
Author(s):  
G.R.L. Feio ◽  
R. Dall’Agnol ◽  
E.L. Dantas ◽  
M.J.B. Macambira ◽  
J.O.S. Santos ◽  
...  
2009 ◽  
Vol 27 (2-3) ◽  
pp. 109-112
Author(s):  
Roberto Dall’Agnol ◽  
Reinhardt A. Fuck ◽  
Raimundo Netuno Nobre Villas

Author(s):  
Ingrid Roberta Viana da Cunha ◽  
Roberto Dall’Agnol ◽  
Bruno Scaillet ◽  
Luan Alexandre Martins de Sousa

2020 ◽  
Vol 104 ◽  
pp. 102817
Author(s):  
Felipe Grandjean da Costa ◽  
Patrick Araújo dos Santos ◽  
Isabelle Cavalcanti Corrêa de Oliveira Serafim ◽  
Iago Sousa Lima Costa ◽  
Sherissa Roopnarain

2017 ◽  
Vol 47 (2) ◽  
pp. 275-299 ◽  
Author(s):  
Bruna Karine Correa Nogueira ◽  
Paulo Sergio de Sousa Gorayeb ◽  
Elton Luiz Dantas ◽  
Rafael Estumano Leal ◽  
Marco Antonio Galarza

ABSTRACT: The São Luís Cráton comprises an area between northeast Pará state and northwest Maranhão that exposes Paleoproterozoic granitic suites and meta-volcanosedimentary sequences. In the east of this geotectonic unit, about 70 km south of São Luís, there is a portion of the São Luís Craton, represented by the intrusive Rosario Suite (RS). This work is focused on rocks of this suite, including petrographic, lithochemical and geochronological studies to understand the crustal evolution of these granitoid rocks. The rock spectrum varies from tonalitic to granodioritic, quartz dioritic and granitic compositions, and there are partial structural and mineralogical changes related to deformation along transcurrent shear zones. The geochemical studies show granitic metaluminous compositions of the calc-alkaline series with I-type affinity typical of magmatic arc. Rare earth elements show marked fractionation and slight Eu positive or negative anomalies (Eu/Eu* = 0.82 to 1.1). Zircon U-Pb data provided consistent ages of 2165 ± 7 Ma, 2170 ± 7 Ma, 2170 ± 7 Ma, 2161 ± 4 Ma and 2175 ± 8 Ma, dating emplacement of these granitoids as Paleoproterozoic (Rhyacian). Sm-Nd isotopic data provided model ages (TDM) of 2.21 to 2.31 Ga with positive values of εNd +1.9 to +3.2 (t = 2.17 Ga), indicating predominantly Rhyacian crustal sources for the parental magmas, similar to those ones found in other areas of the São Luís Craton. The data, integrated with published geological and geochronological information, indicate the occurrence of an important continental crust formation event in this area. The Paleoproterozoic evolution between 2.17 and 2.15 Ga is related to the Transamazonian orogeny. The granitoids of the Rosario Suite represent the main phase of continental arc magmatism that has continuity in other parts of the São Luís Craton and can be correlated with Rhyacian accretionary magmatism in the northwestern portion of the Amazonian Craton that amalgamated Archean terrains during the Transamazonian orogeny.


2020 ◽  
Vol 102 ◽  
pp. 102696 ◽  
Author(s):  
Fernando Fernandes da Silva ◽  
Davis Carvalho de Oliveira ◽  
Roberto Dall’Agnol ◽  
Luciano Ribeiro da Silva ◽  
Ingrid Viana da Cunha

2021 ◽  
Vol 109 ◽  
pp. 103271
Author(s):  
Aline Costa do Nascimento ◽  
Davis Carvalho de Oliveira ◽  
Luciano Ribeiro da Silva ◽  
Cláudio Nery Lamarão

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