Zoomed-in view of the Central Zone IP chargeability anomaly shown in Figure 1, with a 15.5 mV/V response extending for over 1,200 meters north to south. The mafic intrusion is characterized by a high magnetic response (indicated by closely spaced 20 nT contours), which is strongest on either side of the Central Zone structure. The localized magnetic low within the anomaly may result from demagnetization caused by hydrothermal alteration along the structure
Zoomed-in view of the Central Zone IP chargeability anomaly shown in Figure 1, with a 15.5 mV/V response extending for over 1,200 meters north to south. The mafic intrusion is characterized by a high magnetic response (indicated by closely spaced 20 nT contours), which is strongest on either side of the Central Zone structure. The localized magnetic low within the anomaly may result from demagnetization caused by hydrothermal alteration along the structure