I’m not sure how much graphite there is, I recall reading it somewhere that some schist was graphitic. I think IP resistivity is likely to work, picking up silica veining density.
It wouldn’t be very expensive to run a single test IP line across RAS and see what response we get, then if we can see RAS mineralisation then roll it out elsewhere.
Seismic could also work, but it’s slow and expensive. Mineralisation will pool in dilation zones which should appear as a subtle roll (along the direction of shear displacement which I’m assuming is NW-SE judging by the NE orientation of the RAS shoot plunge).
I’m hoping they announce some kind of strategy to find the next shoot other than just drilling.
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