Geochemical anomalies have been outlined by 2022 soil and rock samples and are closely associated with historically observed locations of iron-carbonate alteration (1980s). Zones of iron-carbonate alteration were described as being structurally constrained but varying in width from 1m to 15m. The geochemical anomaly remains open to the east, with historical iron-carbonate alteration zones overlying a large area of low-moderate airborne magnetic response.
Geochemical anomalies have been outlined by 2022 soil and rock samples and are closely associated with historically observed locations of iron-carbonate alteration (1980s). Zones of iron-carbonate alteration were described as being structurally constrained but varying in width from 1m to 15m. The geochemical anomaly remains open to the east, with historical iron-carbonate alteration zones overlying a large area of low-moderate airborne magnetic response.