Mineral chemical study of U-bearing minerals from the Dominion Reefs,South Africa |
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Authors: | Ulrike Rantzsch Christoph D K Gauert Willem A Van der Westhuizen Isabelle Duhamel Michel Cuney Gerhard J Beukes |
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Institution: | 1.Department of Geology,University of the Free State,Bloemfontein,Republic of South Africa;2.Institut für Mineralogie, Kristallographie und Materialwissenschaft,Universit?t Leipzig,Leipzig,Germany;3.G2R, Nancy-Université, CNRS, CREGU,Vand?uvre-lès-Nancy,France |
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Abstract: | The Neo-Archean Dominion Reefs (~3.06 Ga) are thin meta-conglomerate layers with concentrations of U- and Th-bearing heavy
minerals higher than in the overlying Witwatersrand Reefs. Ore samples from Uranium One Africa’s Rietkuil and Dominion exploration
areas near Klerksdorp, South Africa, were investigated for their mineral paragenesis, texture and mineral chemical composition.
The ore and heavy mineral assemblages consist of uraninite, other uraniferous minerals, Fe sulphides, Ni–Co sulfarsenides,
garnet, pyrite, pyrrhotite, monazite, zircon, chromite, magnetite and minor gold. Sub-rounded uraninite grains occur associated
with the primary detrital heavy mineral paragenesis. U–Ti, U–Th minerals, pitchblende (colloform uraninite) and coffinite
are of secondary, re-mobilised origin as evidenced by crystal shape and texture. Most of the uranium mineralisation is represented
by detrital uraninite with up to 70.2 wt.% UO2 and up to 9.3 wt.% ThO2. Re-crystallised phases such as secondary pitchblende (without Th), coffinite, U–Ti and U–Th phases are related to hydrothermal
overprint during low-grade metamorphism and are of minor abundance. |
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