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Peralkaline granite body of the West Congo Belt (Matadi area, Bas-Congo region, DR Congo): a marker of a 1.0 Ga lithospheric-scale extensional event during long-lived Columbia breakup

dc.contributor.authorDe Grave, J.
dc.contributor.authorVan Den Haute, P.
dc.contributor.authorBehiels, M.
dc.contributor.authorEeckout, S.
dc.contributor.authorGlorie, S.
dc.contributor.authorArchibald, DB.
dc.contributor.authorBaudet, D.
dc.contributor.authorFernandez-Alonso, M.
dc.contributor.authorNseka Mbemba, P.
dc.contributor.authorTack, L.
dc.date2018
dc.date.accessioned2024-03-14T13:20:23Z
dc.date.available2024-03-14T13:20:23Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/12250
dc.languageeng
dc.titlePeralkaline granite body of the West Congo Belt (Matadi area, Bas-Congo region, DR Congo): a marker of a 1.0 Ga lithospheric-scale extensional event during long-lived Columbia breakup
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeGeodynamics and mineral resources
dc.source.titleCAG27 Portugal, Aveiro
dc.source.volumeabstracts
dc.source.page67
Orfeo.peerreviewedNo
dc.identifier.rmca5557


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