The jasperoidal cherts at Yarlarweelor could be an Au VMS. But Wodger, who knows?
Typically, though, Au VMS's are very low in Cu and lower-temperature, more toward the epithermal end of the spectrum. They are also fairly rare. The best examples come from the Read volcanic belt in Tasmania, and would look nothing like this (from what has been seen so far). So I wouldn't panic.
The jasperoidal cherts at Yarlarweelor could be an Au VMS. But...
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