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

dc.contributor.author	Oliveira, E.
dc.contributor.author	Souza, Z..
dc.contributor.author	McNaughton, Neal
dc.contributor.author	Lafon, J.
dc.contributor.author	Costa, F.
dc.contributor.author	Figueiredo, A.
dc.date.accessioned	2017-01-30T12:06:31Z
dc.date.available	2017-01-30T12:06:31Z
dc.date.created	2012-03-15T20:01:01Z
dc.date.issued	2011
dc.identifier.citation	Oliveira, E.P. and Souza, Z.S. and McNaughton, N.J. and Lafon, J.-M. and Costa, F.G. and Figueiredo, A.M. 2011. 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. 19: pp. 735-750.
dc.identifier.uri	http://hdl.handle.net/20.500.11937/18213
dc.identifier.doi	10.1016/j.gr.2010.06.005
dc.publisher	Elsevier Science BV
dc.title	The Rio Capim volcanic–plutonic–sedimentary belt, São Francisco Craton, Brazil: Geological, geochemical and isotopic evidence for oceanic arc accretion during Palaeoproterozoic continental collision
dc.type	Journal Article
dcterms.source.volume	19
dcterms.source.startPage	735
dcterms.source.endPage	750
dcterms.source.issn	1342-937X
dcterms.source.title	Gondwana Research
curtin.department	John de Laeter Centre for Mass Spectrometry (COE)
curtin.accessStatus	Fulltext not available