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dc.contributor.authorDe Putter, T.
dc.contributor.authorLiégeois, J.P.
dc.contributor.authorDewaele, S.
dc.contributor.authorCailteux, J.
dc.contributor.authorBoyce, A.
dc.contributor.authorMees, F.
dc.coverage.spatialAfrica - Central
dc.coverage.temporalPaleoproterozoic
dc.date2018
dc.date.accessioned2024-03-14T13:16:27Z
dc.date.available2024-03-14T13:16:27Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/12133
dc.descriptionThe Kisenge-Kamata manganese deposit (Katanga, D.R. Congo) belongs to a group of Paleoproterozoic sedimentary manganese ore occurrences that have been recognized for various parts of Africa. It is a relatively small deposit with total estimated reserves of ∼12 Mt ore, but it is of major importance for understanding key aspects of the geology of the Kasai Block of the Congo Craton. The available constraints indicate that the deposit formed in the 2.0 1.9 Ga time interval, in the Orosirian period. The manganese-rich facies of the Kisenge-Kamata deposits range in composition from manganese carbonate rocks to non-calcareous deposits dominated by manganese- rich garnet. Associated rocks are mainly grey graphitic shales. The Kisenge-Kamata sediments are significantly enriched in Cu, Co, Ni, Zn and other accessory metals (V, Mo, Ga). Field constraints and geochemical data suggest that the Kisenge-Kamata sediments were probably deposited in a relatively small intracratonic basin (graben) within the Kasai Block, with an inlet allowing periodical access for ocean water influx carrying Mn, REE and other metals. Primary carbonate ore has relatively low δ13C (−3 to −6 ) and high δ18O (+13 to +20 ) values, confirming their derivation from marine fluids.
dc.languageeng
dc.publisherElsevier
dc.titlePaleoproterozoic manganese and base metals deposits at Kisenge-Kamata (Katanga, D.R. Congo)
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeGeodynamics and mineral resources
dc.subject.freeSurface environments and collection management
dc.source.titleOre Geology Reviews
dc.source.volume96
dc.source.page181-200
Orfeo.peerreviewedYes
dc.identifier.doihttps://doi.org/10.1016/j.oregeorev.2018.04.015
dc.identifier.rmca5356


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