Am I missing something ?
This early thread stresses the importance of having sulphides in the core. Opaline calls it the "Eldorado"
In the presentation, Churchill Dam Hole 1 is described as having - 150 metres of brecciated and hematite altered GRV intersected with visible sulphides.
I believe that this is the first reference to visible sulphides and surely this is a big plus for the share.
Where am I going wrong ?
Cheers
Armour
gravity anomaly mapping 101, page-9
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