No significant gold or copper intervals were intersected below 830m depth @ rio14 Feb 2022 21:59
But from the RNS:
Visible gold is identified at 1,216m and zones of porphyry-style mineralisation in the form of a notable increase in sulphide mineralisation in magmatic breccias and B-type quartz veins, containing pyrite-chalcopyrite-molybdenite occurs from 1,260-1,680m depth.
Anyone able to make sense of these 2 bits of info?