Personeelslijst
Max Fernandez-Alonso
Aardwetenschappen
Geodynamica en minerale rijkdommen
Geodynamica en minerale rijkdommen
Beschrijving
Dewaele, S., Fernandez-Alonso, M. & Tack, L. 2008. ‘Cassiterite and columbo-tantalite (Coltan) mineralisation in the Proterozoic rocks of the northern part of the Kibara orogen (Central Africa): preliminary results’. Bull. Scéanc. Acad.R. Sci. Outre-Mer 54: 341-357. Brussel : Royal Academy for Overseas Sciences. ISSN: 0001-4176. (PR).
Article in a scientific Journal / Article in a Journal
The Central African Kibara orogen extends from the southeastern part of
Uganda to the southern part of the Democratic Republic of Congo (DRC). It forms a met- allogenic
province that hosts different types of granite-related mineralization: cassiterite,
columbite-tantalite, wolframite, gold, monazite, amblygonite, beryl, etc. These minerals are
present in different types of mineralization. The minerals occur as primary mineraliza- tion in
quartz veins and pegmatites, but also as secondary mineralization in alluvial or elu- vial
deposits. In this study, we focus on the metallogeny of the primary tin and columbite- tantalite
mineralization in the northern part of the Kibara orogen (Rwanda, Burundi, Uganda, Tanzania,
Maniema and Kivu in the DRC). Based on a systematic overview of mining data in the archives of the
RMCA, field work, petrography, geochemical, miner- alogical and microthermometric investigations of
ore and gangue minerals and based on a comparison with recent ore-forming models of granite-related
ore deposits, a preliminary metallogenic model is proposed.
The main granite generation G1-3 intruded at 1380 +/- 10 Ma in the Palaeo- and Mesoproterozoic
rocks of the Kibara orogen. At ~986 Ma, the youngest G4 granite gener- ation formed. Although
historically called “tin”-granite, this granite generation is not min- eralized. After
consolidation of the G4-granite, pegmatites were emplaced (~ 960 Ma). Some of these pegmatites are
mineralized in columbite-tantalite. At ~940 Ma, cassiterite- mineralized quartz veins formed. In
the pegmatite area, this hydrothermal phase resulted
in an intense alteration of the pegmatitic bodies.