Hmmm. I don't think that's covellite. I'd say it's tarnished bornite...are they implying supergene enrichment?? Anyway...
According to the reported logs these are the zones with potentially economic Cu grade:
DD21EB0018W1:
808.07-810.03m - 2 metres
828.9-837.5m - 8.6 metres
DD21EB0018W2:
805.4-806.5m - 1.1 metres
816.2-839.0m - 22.8 metres
So it's shaping up as if there's 2 flat-lying mineralized zones: A very narrow upper zone chalcocite mineralisation (1 to 6 metres width) and a lower, wider zone with bornite-chalcopyrite zone (8 to 36 metres width). The barren to low grade zone that separates the 2 mineralized zones is 8 to 20 metres thickness.
The biggest challenges are depth, Cu grade and shape of the mineralisation
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