The Rio Capim volcanic-plutonic-sedimentary belt, São Francisco Craton, Brazil: Geological, geochemical and isotopic evidence for oceanic arc accretion during Palaeoproterozoic continental collision

Gondwana Research

Volumn 19, Issue 3, 2011, Pages 735-750

  Oliveira, E P ^a   Souza, Z S ^b   McNaughton, N J ^c   Lafon, J M ^d   Costa, F G ^a   Figueiredo, A M ^e  

^a UNIVERSITY OF CAMPINAS   (Brazil)

^b FEDERAL UNIVERSITY OF RIO GRANDE DO NORTE   (Brazil)

^c CURTIN UNIVERSITY   (Australia)

^d FEDERAL UNIVERSITY OF PARÁ   (Brazil)

^e INSTITUTO DE PESQUISAS ENERGÉTICAS E NUCLEARES   (Brazil)

Author keywords

Arc continent collisions; Palaeoproterozoic plate tectonics; Precambrian oceanic arcs; S o Francisco craton

Indexed keywords

ACCRETION; ARC-CONTINENT COLLISION; CONTINENTAL COLLISION; DEFORMATION; GEOCHEMISTRY; ISLAND ARC; ISOTOPIC ANALYSIS; MAGMA; PLATE TECTONICS; PLUTON; PROTEROZOIC;

BRAZIL; SAO FRANCISCO CRATON;

EID: 79952070615     PISSN: 1342937X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.gr.2010.06.005     Document Type: Article

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