South Africa has seven uranium provinces scattered across different national provinces and consisting of different ore deposits. As a signatory to the Pelindaba NPT Treaty, the country is required by the International Atomic Energy Agency (IAEA) to develop its own National Nuclear Forensics Library (NNFL). Nuclear forensic science provides an essential tool to examine nuclear and other radioactive materials, as well as provide evidence that the material was out of regulatory control and was being trafficked. Once the nuclear or radioactive material is seized, the identification of the material and determination of its source is of prime importance. One of the key signatures in nuclear forensics is the isotopic analysis of lead (Pb), which can serve as a fingerprint for nuclear materials. The lead isotopic composition varies between the mining locations, depending on the geological settings. In this study, samples were collected from different mines of Mpumalanga Province. Lead isotopic ratios of the uranium ore were determined using inductively coupled plasma mass spectrometer (ICP-MS) PerkinElmer NexION 2000. According to the results of the lead-lead (Pb–Pb) geochemistry, detrital pyrites make up the mineralization of the uranium ore. The isotopic ratios differed among various ore bodies, which could act as their distinct fingerprints. Additionally, this study provided compelling evidence of the differences between BT and ET, and BT and WT samples. But for the ET-WT pair, it suggested that samples were most likely taken from the same mine shaft.
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