Good research wombarrapete, Now pray that the process you described was active over many tens of thousands to a million or so years which would have contributed to the accumulation of coalescing droplets at depth yielding thick intervals of massive sulphides with a high nickel component. (The high nickel grades we know are there. we also know that we have high copper and platinum grades a la Norilsk). It would also be nice if the disseminated blebs and veins constitute halos and nets above consolidated sulphides which merged from prospect to prospect along the entire Cathedrals Belt Structure, and which now accommodates one big massive orebody down plunge of the ultramafics at depth. So, Norilsk, Here comes St. George.
Please excuse my exuberance, this report shows a much better understanding and rationale of the Mt. Alexander camp and exploration plan!
Cheers,
Helmenesh
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