I am very familiar with the Wingina Well deposit. Most of the mineralisation is bound in a brecciated chert and not so much with all sulphide. There is a narrow zone of mineralisation that is shear bound in a dilational zone. The phyrrotite does not suggest there is 94m of Au as the hydrothermally brecciated chert is the better indicator. That been said the tenements are absolute class with platnium group mineralisation nearby and all other sorts of things. Huge potential if they get back on the path of Geoff Blackburn and D O meara had when de grey started out.
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