Schematic integration of IP chargeability and gravity anomalies at Ranoke, shown on a 1VD magnetic base map. The IP anomaly on Line 1 is 1.1 kilometres across, as shown in Figure 2; also shown on Figure 2 is the profile across the 4 kilometre wide gravity anomaly. The IP anomaly is shallowest in the western part of both Lines 2 and 3; the southeast plunge of the integrated IP anomaly on all 3 lines correlates directly with the high-density body defined in the Company’s 3-D inversion block model of the gravity survey data.
Schematic integration of IP chargeability and gravity anomalies at Ranoke, shown on a 1VD magnetic base map. The IP anomaly on Line 1 is 1.1 kilometres across, as shown in Figure 2; also shown on Figure 2 is the profile across the 4 kilometre wide gravity anomaly. The IP anomaly is shallowest in the western part of both Lines 2 and 3; the southeast plunge of the integrated IP anomaly on all 3 lines correlates directly with the high-density body defined in the Company’s 3-D inversion block model of the gravity survey data.