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A dozen uranium occurrences are known in the Western Zambian Copperbelt (Domes region, Zambia). The host-rocks, Neoproterozoic kyanite±talc micaschists, have been interpreted as meta-evaporites that formed part of an epicontinental sequence affected by upper amphibolite metamorphism during the Pan-African orogeny. Ca–Na metasomatism, expressed by the presence of apatite, epidote and scapolite, is...
The Katanga Copperbelt, in the southeastern part of the Democratic Republic of the Congo (DRC), occurs within the Pan-African Lufilian fold-and-thrust belt and hosts numerous uraniferous mineral occurrences in addition to the world-class sediment-hosted copper and cobalt ore deposits. In the 1950s and 1960s, Cahen et al. gave a relatively wide range of U mineralization ages, using U–Pb dating on whole-rock...
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