Please use this identifier to cite or link to this item: http://www.repositorio.ufop.br/handle/123456789/3949
Title: New U-Pb ages and lithochemical attributes of the Ediacaran Rio Doce magmatic arc, Araçuaí confined orogen, southeastern Brazil.
Authors: Gonçalves, Leonardo Eustáquio da Silva
Farina, Federico
Lana, Cristiano de Carvalho
Soares, Antônio Carlos Pedrosa
Alkmim, Fernando Flecha de
Nalini Júnior, Hermínio Arias
Keywords: Rio Doce arc
Rhyacian basement
Araçuaí-West Congo orogen
Issue Date: 2014
Citation: GONÇALVES, L. E. da et al. New U-Pb ages and lithochemical attributes of the Ediacaran Rio Doce magmatic arc, Araçuaí confined orogen, southeastern Brazil. Journal of South American Earth Sciences, v. 52, p. 129-148, 2014. Disponível em: <http://www.sciencedirect.com/science/article/pii/S0895981114000273>. Acesso em: 04 set. 2014.
Abstract: The Araçuaí orogen of southeastern Brazil, together with its counterpart located in Africa, the West Congo belt, formed through closure of a gulf connected to the Adamastor Ocean by the end of the Ediacaran and beginning of the Cambrian. Convergence of the margins of the gulf led to the development of the Rio Doce magmatic arc between 630 Ma and 580 Ma on a continental basement mostly composed of Rhyacian orthogneisses. The Rio Doce arc mainly consists of tonalite-granodiorite batholiths, generally crowded with mafic to dioritic enclaves, and minor gabbronorite-enderbite-charnockite plutons, suggesting mixing processes involving crustal and mantle sources. We investigate the basement, magma sources and emplacement ages of the Rio Doce arc. Our data suggest the arc comprises three main granitic rock groups: i) Opx-bearing rocks mostly of enderbite to charnockite composition; ii) enclaverich tonalite-granodiorite (ETG); and iii) enclave-poor granite-granodiorite with minor tonalite (GT). The Opx-bearing rocks are magnesian, calc-alkalic to alkali-calcic and metaluminous. Together, the ETG and GT rock groups range in composition from tonalite to granite, are metaluminous to slightly peraluminous, show a predominantly medium- to high-K, expanded calc-alkaline signature, and other geochemical and isotopic attributes typical of a pre-collisional volcanic arc formed on a continental margin setting. Mineralogical, chemical, and geochronological data suggest the involvement of HTmelting of granulitic (H2O-depleted) sources of Rhyacian age for the generation of Opx-bearing granitic rocks, additionally to magma mixing and fractional crystallization processes. In conclusion, the studied rock groups of the Rio Doce arc were likely formed by interactions of mantle and crustal processes, in an active continental margin setting. These processes involved ascent of mantle magmas that induced partial melting on the continental basement represented by the Rhyacian gneisses.
URI: http://www.repositorio.ufop.br/handle/123456789/3949
metadata.dc.identifier.doi: https://doi.org/10.1016/j.jsames.2014.02.008
ISSN: 0895-9811
metadata.dc.rights.license: O periódico Journal of South American Earth Sciences concede permissão para depósito deste artigo no Repositório Institucional da UFOP. Número da licença: 3466021045230.
Appears in Collections:DEGEO - Artigos de periódicos

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