Top Pane: an oblique view of the 1D LEI resistivity inversion voxel for Reveille derived from the high resolution VTEM+ airborne survey flown in June, 2020. Superimposed on the left side are the magnetic isopleths in red and yellow from the MVI 3D inversion model of magnetic data. The 4 drill holes shown are to 300m depth, and are referenced in Figure 1. Lower Pane: an east-west schematic cross-section showing the relationship between the high-grade but distal silver-copper mineralization at the historic Zebra working in the Reveille range to the new and covered T3 and T1 conductors and adjacent magnetic anomaly which both occur along the northeast-southwest trending structure that controls mineralizing fluids at Reveille, as shown on Figure 1.
Top Pane: an oblique view of the 1D LEI resistivity inversion voxel for Reveille derived from the high resolution VTEM+ airborne survey flown in June, 2020. Superimposed on the left side are the magnetic isopleths in red and yellow from the MVI 3D inversion model of magnetic data. The 4 drill holes shown are to 300m depth, and are referenced in Figure 1. Lower Pane: an east-west schematic cross-section showing the relationship between the high-grade but distal silver-copper mineralization at the historic Zebra working in the Reveille range to the new and covered T3 and T1 conductors and adjacent magnetic anomaly which both occur along the northeast-southwest trending structure that controls mineralizing fluids at Reveille, as shown on Figure 1.