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Geochemistry of Li-bearing aplite-pegmatite veins from Cabeço Queimado and associated rocks (Segura, Central Portugal)

dc.contributor.authorAntunes, I.M.H.R.
dc.contributor.authorNeiva, A.M.R.
dc.contributor.authorSilva, M.M.V.G.
dc.contributor.authorRamos, J.M.F.
dc.contributor.authorSilva, P.B.
dc.date.accessioned2011-07-27T14:04:05Z
dc.date.available2011-07-27T14:04:05Z
dc.date.issued2009
dc.description.abstractAt Segura area, two-mica granite, muscovite granite, granitic aplite veins and Libearing granitic aplite-pegmatite veins from Cabeco Queimado intruded the Cambrian schist-metagraywacke complex. Aplite veins also intruded both granites. Variation diagrams of major and trace elements of the granitic rocks show fractionation trends for: a) two-mica granite and Li-bearing aplite-pegmatite veins; b) muscovite granite and aplite veins. Least square analysis for major elements and modelling of trace elements indicate that: a) the Li-bearing aplite-pegmatite veins were derived from the two-mica granite by factional crystallization of quartz, plagioclase, potash feldspar and biotite; b) the aplite veins were derived from muscovite granite by fractional crystallization of quartz, plagioclase, potash feldspar and ilmenite, which is supported by the similar δ18O values. The increase of δ18O values from two-mica granite to aplite-pegmatite veins suggests that fractional crystallization was accompanied by assimilation of metasedimentary material (AFC process). The pegmatite veins are REL-Li pegmatites and belong to the LCT family. The occurrence of amblygonite-montebrasite, lepidolite, cassiterite, ferrocolumbite, manganocolumbite and microlite suggest that Li-bearing granitic aplite-pegmatite veins are highly differentiated.por
dc.identifier.citationANTUNES, I.M.H.R. [et al] (2009) - Geochemistry of Li-bearing aplite-pegmatite veins from Cabeço Queimado and associated rocks (Segura, Central Portugal). Estudos Geológicos. ISSN 1980-82-08. 19:2, p. 40-44.por
dc.identifier.urihttp://hdl.handle.net/10400.11/761
dc.language.isoporpor
dc.peerreviewedyespor
dc.publisherDepartamento de Geologia. Universidade Federal de Pernambucopor
dc.relation.publisherversionhttp://www.ufpe.br/estudosgeologicos/por
dc.subjectLi-bearing aplite-pegmatitespor
dc.subjectCrystal fractionationpor
dc.subjectAn-Nb-Ta oxide mineralspor
dc.titleGeochemistry of Li-bearing aplite-pegmatite veins from Cabeço Queimado and associated rocks (Segura, Central Portugal)por
dc.typejournal article
dspace.entity.typePublication
oaire.citation.conferencePlacePernanbucopor
oaire.citation.titleEstudos Geológicospor
person.familyNameantunes
person.givenNameIsabel Margarida
person.identifier.ciencia-idCB1E-FAD2-37D6
person.identifier.orcid0000-0003-3456-5926
person.identifier.ridM-1043-2013
person.identifier.scopus-author-id6701817085
rcaap.rightsopenAccesspor
rcaap.typearticlepor
relation.isAuthorOfPublication1db83c95-f80c-41bb-b5c6-437ab32d9683
relation.isAuthorOfPublication.latestForDiscovery1db83c95-f80c-41bb-b5c6-437ab32d9683

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