Cross section A-B. Drill holes shown were historically proposed and permitted by Vale but never drilled. Low magnetic susceptibility is interpreted as Phyllic alteration. High chargeability anomalies are interpreted to represent disseminated sulphide associated with a porphyry system. High resistivity is interpreted to result from silica within altered rocks. See Figure 2 for location of section.
Cross section A-B. Drill holes shown were historically proposed and permitted by Vale but never drilled. Low magnetic susceptibility is interpreted as Phyllic alteration. High chargeability anomalies are interpreted to represent disseminated sulphide associated with a porphyry system. High resistivity is interpreted to result from silica within altered rocks. See Figure 2 for location of section.