Hi aubin,
Thanks for your informative post. Agreed, that it is a complicated system and I do like the similarity and apparent continuity of the geology across the GAL and GSR-CNJ tenements - PGE's will not worry about tenement boundaries...... I must that say that I am swaying towards the Plat-Reef type analogue for Mount Thirsty where the ultramafics are sulphur (S) saturated prior to emplacement.
Perhaps Mount Thirsty has a primary PGE Plat-Reef type system with a secondary, black shale/shale PGE bonus. I do not think either GAL or GSR-CNJ have PGE assays back for any of the heavily disseminated sulphides intersections in the black shale/shale yet, so those are going to be very interesting and may be the icing on the cake if its lateral / areal extent is predictable and broad i.e. km2.
Kind regards OldGeo
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