Outline of the 3.5 mGal gravity anomaly shown in Figure 1, and contours for the MVI magnetic inversion anomaly, plotted on an RTP magnetic base map. The anomalies are discordant to the RTP magnetic patterns which relate to the primary emplacement of the multi-phase complex at H-K. As such, high density REE mineralization is believed to be related to an evolved fluid late in the formation of an extensive, sulfide-bearing, fluorite-carbonate IOCG hydrothermal breccia system that is hosted within, but is destructive to, the original phases of the complex.
Outline of the 3.5 mGal gravity anomaly shown in Figure 1, and contours for the MVI magnetic inversion anomaly, plotted on an RTP magnetic base map. The anomalies are discordant to the RTP magnetic patterns which relate to the primary emplacement of the multi-phase complex at H-K. As such, high density REE mineralization is believed to be related to an evolved fluid late in the formation of an extensive, sulfide-bearing, fluorite-carbonate IOCG hydrothermal breccia system that is hosted within, but is destructive to, the original phases of the complex.