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dc.creatorZaccarini, F.-
dc.creatorGaruti, G.-
dc.creatorMartín, R. F.-
dc.date2008-06-12T07:52:22Z-
dc.date2008-06-12T07:52:22Z-
dc.date2006-
dc.date.accessioned2017-01-31T01:39:55Z-
dc.date.available2017-01-31T01:39:55Z-
dc.identifierGeologica acta: an international earth science journal, Vol. 4, Nº. 4, 2006 , pags. 461-469-
dc.identifier1695-6133-
dc.identifierhttp://hdl.handle.net/10261/5018-
dc.identifier.urihttp://dspace.mediu.edu.my:8181/xmlui/handle/10261/5018-
dc.descriptionThe Campo Formoso stratiform intrusive complex, in Bahia State, Brazil, considered to be Paleoproterozoic age consist of a tabular body of ultramafic rocks about 40 km log and 100-1100 m. wide. Thick horizons of chromitite are exploited and the deposits are the richest in Brazil. The complex was intruded by the Campo Formoso calc-alkaline batholith, emplaced by the result of the Transamazonian collision-realated orogeny.-
dc.descriptionPeer reviewed-
dc.format298970 bytes-
dc.formatapplication/pdf-
dc.languageeng-
dc.publisherCSIC - Instituto de Ciencias de la Tierra Jaume Almera (ICTJA)-
dc.rightsopenAccess-
dc.subjectCampo Formoso-
dc.subjectChromitites-
dc.subjectMonazite-
dc.subjectApatite-
dc.subjectPb-D-Sb bearing minerals-
dc.subjectBrazil-
dc.titleExotic accesory minerals in layered chromitites of the Campo Formoso complex (Brazil)-
dc.typeArtículo-
Appears in Collections:Digital Csic

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