Property-scale RTP magnetic plan map showing the large and prominent magnetic anomaly located at the southwest end of the structural corridor that controls the high-grade silver-copper mineralization at the Zebra showing. The geometry of the magnetic-low alteration halo to this anomaly is consistent with the northeast-trending fold axis that defines the structural trend and fluid pathway to Zebra. The geochemical vector shown for Zn/Pb, a proxy for high temperature, is based on more than 190 samples collected by VR in 2020, and is consistent with the vectors for other high temperature minerals such as tungsten, and for silver, copper and gold which are shown in Figures 1 and 3. Geochemical vectors indicate that this magnetic anomaly is the potential high temperature core and driver to the overall CRD silver-copper mineral system at Reveille.
Property-scale RTP magnetic plan map showing the large and prominent magnetic anomaly located at the southwest end of the structural corridor that controls the high-grade silver-copper mineralization at the Zebra showing. The geometry of the magnetic-low alteration halo to this anomaly is consistent with the northeast-trending fold axis that defines the structural trend and fluid pathway to Zebra. The geochemical vector shown for Zn/Pb, a proxy for high temperature, is based on more than 190 samples collected by VR in 2020, and is consistent with the vectors for other high temperature minerals such as tungsten, and for silver, copper and gold which are shown in Figures 1 and 3. Geochemical vectors indicate that this magnetic anomaly is the potential high temperature core and driver to the overall CRD silver-copper mineral system at Reveille.