Late Neoproterozoic-Cambrian granitic magmatism in the Araçuaí orogen (Brazil), the Eastern Brazilian Pegmatite Province and related mineral resources

AC Pedrosa-Soares, CP De Campos… - Geological Society …, 2011 - lyellcollection.org
The Araçuaí orogen extends from the eastern edge of the São Francisco craton to the
Atlantic margin, in southeastern Brazil. Orogenic igneous rocks, formed from c. 630 to c. 480 …

Similarities and differences between the Brazilian and African counterparts of the Neoproterozoic Araçuaí-West Congo orogen

AC Pedrosa-Soares, FF Alkmim, L Tack… - Geological Society …, 2008 - lyellcollection.org
The Araçuaí–West Congo orogen encompasses orogenic domains located to the SE of the
São Francisco Craton in Brazil, and to the SW of the Congo Craton in Africa. From the …

The Ediacaran Rio Doce magmatic arc revisited (Araçuaí-Ribeira orogenic system, SE Brazil)

M Tedeschi, T Novo, A Pedrosa-Soares, I Dussin… - Journal of South …, 2016 - Elsevier
Described half a century ago, the Galiléia tonalite represents a milestone in the discovery of
plate margin magmatic arcs in the Araçuaí-Ribeira orogenic system (southeastern Brazil). In …

[PDF][PDF] Orógeno Araçuaí: síntese do conhecimento 30 anos após Almeida 1977

AC Pedrosa-Soares, CM Noce, F Alkmim, LC Silva… - Geonomos, 2007 - repositorio.usp.br
The Araçuaí Fold Belt was defined as the southeastern limit of the São Francisco Craton in
the classical paper published by Fernando Flávio Marques de Almeida in 1977. This …

The São Francisco Palaeocontinent

AN Sial, MA Dardenne, A Misi, AJ Pedreira… - … in Precambrian Geology, 2009 - Elsevier
The São Francisco and the Congo cratons represent sectors of a Neoproterozoic
palaeocontinent preserved from the Brasiliano-Pan African orogeny, recorded in their …

From the plutonic root to the volcanic roof of a continental magmatic arc: a review of the Neoproterozoic Araçuaí orogen, southeastern Brazil

L Gonçalves, FF Alkmim, A Pedrosa-Soares… - International Journal of …, 2018 - Springer
The Araçuaí-West Congo orogen (AWCO) is one of the various components of the
Brasiliano/Pan-African orogenic network generated during the amalgamation of West …

Juvenile contribution of the Neoproterozoic Rio Negro magmatic arc (Ribeira Belt, Brazil): implications for western Gondwana amalgamation

M Tupinambá, M Heilbron, C Valeriano, RP Júnior… - Gondwana …, 2012 - Elsevier
The ca. 790–600Ma Rio Negro Complex (RNC) of the Ribeira belt (Brazil) consists of a
plutonic portion of a magmatic arc built by the E-vergent subduction of the ESE border of the …

Tectonic evolution of the Juvenile Tonian Serra da Prata magmatic arc in the Ribeira belt, SE Brazil: Implications for early west Gondwana amalgamation

C de Araujo Peixoto, M Heilbron, D Ragatky… - Precambrian …, 2017 - Elsevier
The evolution of the Ribeira belt resulted from the progressive amalgamation of several
terranes against the eastern margin of the São Francisco Craton between ca. 620 and 580 …

Granites of the intracontinental termination of a magmatic arc: an example from the Ediacaran Araçuaí orogen, southeastern Brazil

L Gonçalves, FF Alkmim, AC Pedrosa-Soares… - Gondwana …, 2016 - Elsevier
The Araçuaí orogen of southeastern Brazil together with the West Congo belt of central West
Africa form the Araçuaí–West Congo orogen generated during closure of a terminal segment …

The Serra da Bolívia complex: the record of a new Neoproterozoic arc-related unit at Ribeira belt

M Heilbron, M Tupinambá… - Precambrian …, 2013 - Elsevier
The Neoproterozoic arc related rocks of the central segment of the Ribeira belt crop out at
the Oriental Terrane that is subdivided into three thrust sheets verging northwestern ward …