A large 0.5 to 1 million oz deposit underlying the mineralisation at surface, which is
persistent but widely dispersed within the well-defined 300-400m wide mineralise corrider.
The minseralisation targeted is at depth of 200-300m. The minseralisation is pyrite-arsenopyrite rich and occurs in pods, lenses and discontinous veins making it ideally suited to detection by IP electrical survey. The metallurgy is not dissimilar to that of the Majors Creek deposit near Braidwood which may indicate an intrusive source.
Geology: hosted by Ordovician metasediments (similar host rocks to Bendigo and Fosterville)