Black Lake South Project

The Northern Athabasca Black Lake South Project spans an area of 49.4 sq km and features a classic unconformity uranium deposit model, akin to the one observed at Key Lake, with deposits located at shallow depths. Numerous electromagnetic (EM) anomalies have been identified, believed to be bedrock graphitic conductors crucial for the genesis of unconformity-style uranium deposits. These conductors coincide with robust uranium radiometric anomalies, further bolstering the validity of the target model. Significantly, these conductors are closely associated with a pelitic biotite-amphibole gneiss unit known to harbor graphitic horizons pivotal for deposit formation.