Tray photograph and gold grades of the Kiwi Zone in drillhole BD513. The mineralisation is quartz-dominated in contrast to the upper Brunswick South structure, and occurs at a low angle to the west-dipping bedding, following the Kiwi Fault plane. This is dissimilar to K-R mineralisation beneath Brunswick Main where vertical veins are bound between the hangingwall and footwall planes of the fault slice due to the flattening of the Kiwi and Rooster Fault structures, being more aligned with a Youle-like geometry.
Tray photograph and gold grades of the Kiwi Zone in drillhole BD513. The mineralisation is quartz-dominated in contrast to the upper Brunswick South structure, and occurs at a low angle to the west-dipping bedding, following the Kiwi Fault plane. This is dissimilar to K-R mineralisation beneath Brunswick Main where vertical veins are bound between the hangingwall and footwall planes of the fault slice due to the flattening of the Kiwi and Rooster Fault structures, being more aligned with a Youle-like geometry.