EPL3670 is considered to be prospective for both, primary and secondary (surficial) uranium mineralization. Leucogranites under cover are believed to host primary ‘Rossing’-style uranium mineralization, in particular along favorable lithostratigraphic contacts. The Cenozoic sediment cover has potential to host surficial ‘Langer Heinrich’-style uranium mineralization. Airborne EM data indicates the existence of NNE-SSW trending drainages. Isolated uranium anomalies over the Cenozoic succession on EPL3670 support this mineralization model.
Prpject status APPROVED
Ministry of Environment and Tourism
Department of Environmental Affairs
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