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Coupled silicon-oxygen isotopic evidences for the origin of silicification in mafic volcanic rocks of the Barberton Greenstone Belt.

dc.contributor.authorAbraham, K.
dc.contributor.authorHofmann, A.
dc.contributor.authorFoley, S.F.
dc.contributor.authorCardinal, D.
dc.contributor.authorHarris, C.
dc.contributor.authorBarth, M.
dc.contributor.authorAndré, L.
dc.date2011
dc.date.accessioned2016-03-15T10:04:49Z
dc.date.available2016-03-15T10:04:49Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/1031
dc.languageeng
dc.titleCoupled silicon-oxygen isotopic evidences for the origin of silicification in mafic volcanic rocks of the Barberton Greenstone Belt.
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeSurface environments and collection management
dc.source.titleEarth and Planetary Sci. Lett.,
dc.source.volume301
dc.source.page222-230
Orfeo.peerreviewedYes
dc.identifier.rmca2443


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