Figure 3

Figure 3

Photograph and select geochemistry from a hand sample of hydrothermal iron oxide breccia composed of massive hematite with disseminated pyrite discovered in a riverbed 12 kilometres south of the Ranoke anomaly. The low magnetic susceptibility high resistivity, chargeability (IP) and density measured in this sample by VR are compatible with the IP, resistivity and gravity anomalies shown in Figures 1 and 2, within a zone of low magnetic intensity. This underscores the potential for an iron oxide copper-gold breccia pipe at Ranoke.

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PNG

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VR Resources

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