"Mineralisation at the Colosseum mine is primarily contained in two breccia pipes that are made up of a combination of sediment, felsite and granite units.
Until recently, very high grade mineralisation was thought to occur only in the sedimentary breccia unit.
Drill holes CM24-16 and CM24-15 have demonstrated high grade mineralisation can also occur in the felsite breccia unit.
In addition, drill hole CM23-14 intersected mineralisation in quartz veins that are in the granite outside of the breccia pipes.
A revised geology model will be completed when the balance of the results from CM24-16 become available."
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