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Fluid fractionation of tungsten during granite pegmatite differentiation and the metal source of peribatholitic W quartz veins: Evidence from the Karagwe-Ankole Belt (Rwanda)

dc.contributor.authorHulsbosch, N.
dc.contributor.authorBoiron, M.C.
dc.contributor.authorDewaele, S.
dc.contributor.authorMuchez, Ph.
dc.date2016
dc.date.accessioned2016-03-15T10:08:01Z
dc.date.available2016-03-15T10:08:01Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/2658
dc.languageeng
dc.publisherElsevier Ltd
dc.titleFluid fractionation of tungsten during granite pegmatite differentiation and the metal source of peribatholitic W quartz veins: Evidence from the Karagwe-Ankole Belt (Rwanda)
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freePROMINES
dc.source.titleGeochimica et Cosmochimica Acta
dc.source.volume175
dc.source.page299-318
Orfeo.peerreviewedYes
dc.identifier.urlhttp://dx.doi.org/10.1016/j.gca.2015.11.020
dc.identifier.rmca4499


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