This is good looking stuff. The bornite in foliated ultramafic is particularly strange, as VMS's aren't generally formed in ultramafic, although the Evelyn deposit near Whim Creek is hosted in Archaean ultramafics with dacite cryptodomes. Here, mineralisation is pre at least one deformation, which is clearly a bit different than what I was assuming when I associated this even with Thaduna...depending on whether the bornite is replacing carbonate veining in the ultramafic or not.
Needs a few more stiff long blacks and a bit of a chin scratch!
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