The main DeGrussa deposit represents a 20 m-thick, steeply dipping to almost vertical body of high grade copper-gold mineralisation with lesser zinc and silver. It is defined over a 180 m lateral strike extent and persists to a known vertical depth of more than 300 m.
The Conductor 1 deposit occurs as a number of stacked lenses and underlies the main DeGrussa ore zone. It averages 15 m in thickness and extends over a lateral strike length of 350 m, with a steep 75° south-west trending dip, persisting to a known vertical depth of 400 m.
The smaller Conductor 4 deposit lies 120 m below and 200 m east of Conductor 1 and DeGrussa. A further small deposit, Conductor 5 has also been delineated, ~200 m further to the east.
All are distributed along the steep, northeast-trending Shiraz Fault zone which offsets the ore bodies and is a significant local structure with varying widths of highly broken material. The Merlot and Pinot faults also have a local, but less pronounced interaction with the massive sulphide lenses.
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