RE:RE:Fission Drilling beyond 1620E Line 2190E – Hole PLS13-040, a vertical hole, was drilled approximately 2.2km to the east along strike of R00E. Bedrock was encountered at 54.5m and consisted of primarily semipelitic and pelitic gneiss (locally graphitic from 86.9 – 97.3m) to 109.5m. A possible mafic rock was encountered from 109.5m to the end of hole (182.0m). Significant clay alteration was present over several intervals from 54.5m to 109.5m, including an interval of sulphide (pyrite) mineralization from 89.0 – 97.3m. Overall uranium values were low ranging from <2ppm to 17ppm, moderately elevated between 83.5m – 106.5m (4ppm – 17ppm), coincident with the interval of sulphide mineralization.
Line 1995E – Hole PLS13-042 a vertical hole was drilled approximately 2.0km east of R00E. Bedrock was encountered at 45.0m and consists of alternating sequences of semipelitic and pelitic gneiss (locally graphitic) to the end of hole at 203.4m. Moderate to strong chlorite alteration is present from the top of the basement to 121.2m. From 121.2m to 200.0m, alternating sequences of moderate to strong chlorite alteration and sulphide mineralization are present throughout. Overall uranium values were low but showing a moderate elevation between 106.0m – 196.5m (4ppm – 59ppm), coincident with the interval of sulphide mineralization.