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1.- The Rio Capim volcanic-plutonic-sedimentary belt, Sao Francisco Craton, Brazil; geological, geochemical and isotopic evidence for oceanic arc accretion during Palaeoproterozoic continental collision
Elsevier on behalf of International Association for Gondwana Research; Amsterdam and Kochi; III; Int, 2011
Island arcs; their role in growth of accretionary orogens and mineral endowment
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