Figure 3: Illustrates the shallow plunge to the northwest of the high-grade mineralization at the South Reef Main and South Reef Upper zones. Importantly the width of the structure and intensity of brecciation that host mineralization is increasing to the northwest on the South Reef Main zone highlighting the potential for additional mineralization. In addition, a high-grade chute is emerging on the South Reef Upper zone demonstrating the prospectivity of the entire structural corridor.
Figure 3: Illustrates the shallow plunge to the northwest of the high-grade mineralization at the South Reef Main and South Reef Upper zones. Importantly the width of the structure and intensity of brecciation that host mineralization is increasing to the northwest on the South Reef Main zone highlighting the potential for additional mineralization. In addition, a high-grade chute is emerging on the South Reef Upper zone demonstrating the prospectivity of the entire structural corridor.