2005
DOI: 10.1016/j.jsames.2004.09.003
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Two neoproterozoic crustal accretion events in the Brasília belt, central Brazil

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Cited by 134 publications
(88 citation statements)
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“…The main metamorphic event took place at ca. 630 Ma, as indicated by U-Pb titanite data and Sm-Nd garnet ages (Laux et al 2005). This is similar to the regional metamorphic event observed in several other parts of the Brasília Belt, and has been interpreted as representative of the final closure of the ocean and continental collision (for a review see Cordani et al 2013).…”
Section: Introductionsupporting
confidence: 77%
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“…The main metamorphic event took place at ca. 630 Ma, as indicated by U-Pb titanite data and Sm-Nd garnet ages (Laux et al 2005). This is similar to the regional metamorphic event observed in several other parts of the Brasília Belt, and has been interpreted as representative of the final closure of the ocean and continental collision (for a review see Cordani et al 2013).…”
Section: Introductionsupporting
confidence: 77%
“…1), the Brasília Belt includes: 1. several metasedimentary units deposited on a Paleoproterozoic sialic basement (Almeida et al 1981, Fuck et al 1993, Pimentel et al 2000; 2. one small allochthonous sialic fragment made dominantly of Archean trondhjemite-tonalite-granodiorite (TTG) terranes and greenstone belts (the Goiás Archean block of Jost et al 2013); 3. three large mafic-ultramafic complexes (Barro Alto, Niquelândia and Cana Brava;Ferreira Filho et al 2010); 4. the Neoproterozoic Goiás Magmatic Arc in the west (for a brief review see Laux et al 2005, Brito-Neves et al 2014); 5. a large Neoproterozoic high-grade terrain known as the Anápolis-Itauçu complex, interpreted as the roots of the Brasília orogen (Piuzana et al 2003.…”
Section: Geological Contextmentioning
confidence: 99%
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“…Its reference age after Jackson et al (2004) For an additional test of the method, two zircon samples from our own laboratory which had previously been dated by other analytical methods were also investigated here. One is a relatively young zircon concentrate (sample HD66) from a hornblende-bearing orthogneiss of the Neoproterozoic Goiás magmatic arc which has previously been dated at 630 ± 5 Ma (2σ ) by U-Pb ID-TIMS in our laboratory (Laux et al 2005 …”
Section: Standards and Samplesmentioning
confidence: 99%
“…Os dados geocronológicos, geoquímicos e isotópicos disponíveis sugerem que o Arco Magmático de Goiás é resultado de um sistema de arcos de ilhas intraoceânicos, caracterizados por tonalitos a dioritos cálcio-alcalinos, e vulcânicas associadas, formados por dois eventos de acreção crustal, um entre ~900 e ~800 Ma e outro entre ~670 a ~600 Ma Laux et al, 2005). Dados isotópicos e geocronológicos apresentados por Rodrigues et al (1999), Pimentel et al (2000) e Navarro et al (2004) estendem a ocorrência de rochas juvenis associadas ao Arco Magmático de Goiás até a região de Pontalina-Burití Alegre (Figura 1).…”
Section: Introductionunclassified