Geological setting
- Intrusive suite cutting the Reguibat Shield basement, dominated by granites and granodiorites.
- Intense fracturing favouring fluid circulation and uranium remobilisation.
- Carnotite formation in weathered near-surface levels and open fractures.
- Well-expressed airborne radiometric anomalies, readily recognised on the ground.
Target mineralisation
- Primary and secondary uranium (U3O8), with carnotite in the weathering zone
- Associated Group 4 radioactive elements
- Copper occurrences and accessory minerals linked to the intrusions
- Gold in neighbouring host formations
Our activity
The Tiferchai area, roughly 130 km east of Nouâdhibou, concentrates our most intensive campaigns: detailed trenching, inclined RC drilling and assaying under a QA/QC plan, with a notable intersection of 431 ppm U3O8 over 13 metres from surface.