Interpretive cross section of holes 21OMI-001 and 21OMI-002. Two levels/episodes of mineralization are evident. The lower system was buried by volcaniclastic material which was, in turn. buried by a rhyolite lava flow. The hydrotherm system re-established itself following these events. Irving believes the lower mineralized system is fertile for discovery and that areas around the Honpi structure could host important precious metal veins.
Interpretive cross section of holes 21OMI-001 and 21OMI-002. Two levels/episodes of mineralization are evident. The lower system was buried by volcaniclastic material which was, in turn. buried by a rhyolite lava flow. The hydrotherm system re-established itself following these events. Irving believes the lower mineralized system is fertile for discovery and that areas around the Honpi structure could host important precious metal veins.