One might have hoped for a bit more of a sniff of gold in all that pyrite bearing skarn alteration. Bottom of hole 4 might be much more interesting with chalcopyrite prevalent and commonly associated with gold in copper-bearing magnetite skarns. Getting pretty deep down there though. Is the source of the eluvials now completely gone being a more epithermal part of the system?
Anyway - a technical success none-the-less with the follow up to the IP. Ongoing modelling of intrusion sourced fluids and alteration of calc-silicates on this project within a highly prospective province should keep them busy.
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