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dc.contributor.authorIlombe, G.M.
dc.contributor.authorMukokya, Y.M.
dc.contributor.authorNzolang, C.
dc.contributor.authorKalikone, C.B.
dc.contributor.authorBirhenjira, E.M.
dc.contributor.authorMugaruka, B.T.
dc.contributor.authorDelvaux, D.
dc.contributor.editorD. Delvaux, C. Michellier, O. Dewitte
dc.coverage.spatialAfrica - Central
dc.coverage.spatialCongo, The Democratic Republic of the
dc.coverage.temporalPrecambrian
dc.date2017
dc.date.accessioned2024-03-14T13:13:56Z
dc.date.available2024-03-14T13:13:56Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/11779
dc.descriptionA geological investigation of the Kibaran series of Kamituga (Kivu Supergroup) was carried out in the Mobale gold deposit at Kamituga with a cartographic, petrographic and structural approach. The petrographic analyses showed the existence of mesozonal metasediments (quarzite and metapelite) affected by a bimodal magmatism, first of dioritic and later of a granitic nature. Two deformation phases affect the metasediments: (D1) a first E-W folding with subhorizontal axis and axial-plane cleavage (S1) of presumed Kibaran age, and (D2) a second N-S folding with an axis moderately inclined towards the South. The latter could represent a Pan-African influence outside the Itombwe Synclinorium and would therefore be the first evidence, for a Pan-African folding affecting the Kibaran series.
dc.languagefra
dc.publisherAfrica Museum
dc.titleGeology and structure of Mobale gold deposit at Kamituga: A contribution to the study of the Kivu Supergroup
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeGeodynamics and mineral resources
dc.source.titleGeo-Eco-Trop
dc.source.volume41/2; Geohazards in the Great Lakes Region of Central Africa
dc.source.page151-168
Orfeo.peerreviewedYes
dc.identifier.urlhttp://www.geoecotrop.be/
dc.identifier.rmca5134


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