Figure 4: Vertical section resistivity and chargeability (inverted) plot of 2024 IP survey line 1200N, looking to the northwest. The geophysical anomaly remains largely untested to depth on line 1200N. Elevated resistivity values are interpreted to indicate zones of brecciation and quartz veining as observed in historical core logs and on surface.
Figure 4: Vertical section resistivity and chargeability (inverted) plot of 2024 IP survey line 1200N, looking to the northwest. The geophysical anomaly remains largely untested to depth on line 1200N. Elevated resistivity values are interpreted to indicate zones of brecciation and quartz veining as observed in historical core logs and on surface.