Redking, diorite could very well be richer. You don't have a dozen surface leeders all plus 100g per tonne just on there own.
There is a large amount of alluvial workings, gold travels down hill, so that may have come from the reefs.
But these refers were small, to small to shed over such a large area.
Often high grade surface leeders bulk up at depth, I've seen this in Victoria.
There are just to many to be individual pockets of reef, reefs just do not work that way.
So somewhere there, under cover will be the source to those reefs and alluvial gold.
Tnr got great surface samples, but there over a large area, so why the tracer minerals to zone in.
Its to big an area to just put holes down hoping.
Mt stirling and Stirling well was not that rich grade, so I agree diorite most interesting.
All we need is one assay and game on there.
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