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Effect and significance of contamination-related compositional melt variations of the Tweerivier and Bulhoekkop carbonatites, South Africa, with special reference to their REE mineralization

Subject Area Mineralogy, Petrology and Geochemistry
Term from 2019 to 2022
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 437542348
 
Final Report Year 2024

Final Report Abstract

Carbonatites represent important rare earth elements (REE) deposits, which is reflected by the fact that REE exploration projects worldwide are dominated by carbonatites and accompanying rock types. The extraordinary REE enrichment in carbonatitic melts is generally attributed to a combination of parameters, including low-degree partial melting of enriched mantle sources, crystal fractionation, separation of fluid phases and hydrothermal alteration. However, the effect of contamination by crustal and cogenetic rocks, as a potential first order process is only weakly constrained. The funded project combines investigations on the Gross Brukkaros, Dicker Willem, Kieshöhe carbonatite complexes in Namibia and the Bulhoek, Tweerevier, Welgevonden, Nooitgedacht and Palabora carbonatite complexes in the Republic of South Africa. The results clearly provide evidence that the interaction of carbonatite magma with silicate wall rocks and xenoliths can significantly influence the REE mineralization of carbonatites. This concerns both the magmatic mineralisation of discrete REE minerals, which can exhibit systematic changes in the type REE minerals occurring with the intensity of contamination (e.g. the specific occurrence of allanite and britholite), and the magmatic mineralisation of REE-bearing minerals, such as apatite, which specifically incorporates REE through contamination (Si involved britholite substitution) and thus depletes the residual melt in REE. Furthermore, hydrothermal postmagmatic processes can also be strongly influenced by the presence of silicates (formed by prior magmatic xenolith input/contamination) during the redistribution of REE, as silica-enriched fluids in the carbonate-rich system possess different ligand properties. The chosen examples mentioned above are known to bear a large variability of crustal xenoliths (BIF, sedimentary dolomites, granites, anorthosites and gabbros but also alkaline igneous rocks) and contain variable amounts of silicate minerals (e.g., amphibole, clinopyroxene, mica, tremolite) that can be related to the effect of crustal contamination. The case study of Gross Brukkaros, Dicker Willem, Welgevonden, Nooitgedacht and Palabora clearly show the influence of crustal contamination by various chemically contrasting contaminants whereas the Kieshöhe case study show the influence of silica-rich xenoliths on the hydrothermal and supergene stages and related REE enrichments. Hence crustal contamination of carbonatite melts is a first order process that needs to be considered at each stage of mineralization and redistribution.

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