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Exotic accesory minerals in layered chromitites of the Campo Formoso complex (Brazil)

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dc.creator Zaccarini, F.
dc.creator Garuti, G.
dc.creator Martín, R. F.
dc.date 2008-06-12T07:52:22Z
dc.date 2008-06-12T07:52:22Z
dc.date 2006
dc.date.accessioned 2017-01-31T01:39:55Z
dc.date.available 2017-01-31T01:39:55Z
dc.identifier Geologica acta: an international earth science journal, Vol. 4, Nº. 4, 2006 , pags. 461-469
dc.identifier 1695-6133
dc.identifier http://hdl.handle.net/10261/5018
dc.identifier.uri http://dspace.mediu.edu.my:8181/xmlui/handle/10261/5018
dc.description The 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.description Peer reviewed
dc.format 298970 bytes
dc.format application/pdf
dc.language eng
dc.publisher CSIC - Instituto de Ciencias de la Tierra Jaume Almera (ICTJA)
dc.rights openAccess
dc.subject Campo Formoso
dc.subject Chromitites
dc.subject Monazite
dc.subject Apatite
dc.subject Pb-D-Sb bearing minerals
dc.subject Brazil
dc.title Exotic accesory minerals in layered chromitites of the Campo Formoso complex (Brazil)
dc.type Artículo


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