IP chargeability and resistivity profiles from Line 1 at the Ranoke property (see line location in Figure 1). Data are from TITAN24 DCIP survey completed by Quantec Geoscience Ltd., September, 2019. The correlation of the chargeability anomaly with high resistivity is consistent with the properties of a cobble of sulfide-bearing iron oxide breccia discovered in a riverbed 12 kilometres to the south of the property (see Figure 3). The gravity profile in the third profile down shows the correlation of the IP anomaly with the center of the gravity anomaly at Ranoke. The lower panel shows the correlation of gravity and IP anomalies with a high-contrast magnetic low zone within the Ranoke magnetic complex.
IP chargeability and resistivity profiles from Line 1 at the Ranoke property (see line location in Figure 1). Data are from TITAN24 DCIP survey completed by Quantec Geoscience Ltd., September, 2019. The correlation of the chargeability anomaly with high resistivity is consistent with the properties of a cobble of sulfide-bearing iron oxide breccia discovered in a riverbed 12 kilometres to the south of the property (see Figure 3). The gravity profile in the third profile down shows the correlation of the IP anomaly with the center of the gravity anomaly at Ranoke. The lower panel shows the correlation of gravity and IP anomalies with a high-contrast magnetic low zone within the Ranoke magnetic complex.