Remobilized copper, gold and silver mineralization occur in shear-hosted chalcopyrite and bornite with strong silicification (pale areas around sulfides) in an amphibolite host. The sample is taken from an exploration trench situated above the newly defined chargeability anomaly shown in Figure 1.
Remobilized copper, gold and silver mineralization occur in shear-hosted chalcopyrite and bornite with strong silicification (pale areas around sulfides) in an amphibolite host. The sample is taken from an exploration trench situated above the newly defined chargeability anomaly shown in Figure 1.