Yeah, and keen punters may be looking for evidence of sulphides from a magmatic source. And you don't really have that described here in a big way beyond the trace amounts that you might normally expect, IMO. And the higher concentrations of sulphide (pyrrhotite) sit in meta-sediments, which you may also expect. So looking forward, one might want to see evidence that those trace base metal sulphides in the gabbro can vector them in to discover a larger cumulate of massive sulphides within the same or similar mafic hosts. That's the story today, IMO. The pyrrhotite and graphite in meta-sediments may prove to be a distraction, particularly in EM. Worth following though - the host potential looks better than that drilled by many players chasing stratigraphic graphite / pyrrhotite lighting up all the VTEM conductors during the great Fraser Range craze of a few years back.
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Yeah, and keen punters may be looking for evidence of sulphides...
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