Hi Shady
yeah that's somewhat how i'm imagining things at the moment. Lens (or fried egg-shaped zones) of Copper rich sulphides minor Au, Ag steeply dipping at ~60 to 80 degrees. Stockwork/stringer zone with Cu on the hanging side; with Pb and Zn sulphides, strong chemical zones on the top. Zn more to the rims and carbonaceous sediments, um, across the top surface then widening broadly, I think.
Haven't got my head around the gold dominated northern conductor yet - and there's a good question someone asked - are the two conductors linked?
I might add another question: are there other conductors nearby?
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