Figure 2: 3D view (looking north from above) The orange “cloud” shows a conductive zone detected by the EM survey. The red and blue outlines are earlier models of denser and more magnetic rock. The anomaly sits beside the Uitloop intrusion and close to those outlines, which fits how massive sulphides often occur: they tend to “pool” along the base or edges of an intrusion or in feeder embayments, slightly offset from the hardest, most magnetic core. This geometry is consistent with that setting, although it does not confirm mineralisation.
Figure 2: 3D view (looking north from above) The orange “cloud” shows a conductive zone detected by the EM survey. The red and blue outlines are earlier models of denser and more magnetic rock. The anomaly sits beside the Uitloop intrusion and close to those outlines, which fits how massive sulphides often occur: they tend to “pool” along the base or edges of an intrusion or in feeder embayments, slightly offset from the hardest, most magnetic core. This geometry is consistent with that setting, although it does not confirm mineralisation.