North-south conductivity profile for 3D-array DCIP survey shown in plan in Figure 1 above, with off-section drill trace for hole NB26-003 at -75 towards 145 azimuth. Host-rock Triassic limestone stratigraphy is north-dipping across the New Boston property. The two IP chargeability bodies range from 15-21 mV/V. NB26-003 targeted the south-plunging conductivity anomaly starting from surface and cross-cutting stratigraphy, into the co-spatial IP root and through the CCT stratigraphic contact below the south flank of Jeep Mine hill. The model is clipped at 500 m depth by convention; there is no bottom to the IP anomaly at Jeep Mine in the inversion model, consistent with the sulfide-bearing veins throughout 2,892 ft of drill core in NB26-003.
North-south conductivity profile for 3D-array DCIP survey shown in plan in Figure 1 above, with off-section drill trace for hole NB26-003 at -75 towards 145 azimuth. Host-rock Triassic limestone stratigraphy is north-dipping across the New Boston property. The two IP chargeability bodies range from 15-21 mV/V. NB26-003 targeted the south-plunging conductivity anomaly starting from surface and cross-cutting stratigraphy, into the co-spatial IP root and through the CCT stratigraphic contact below the south flank of Jeep Mine hill. The model is clipped at 500 m depth by convention; there is no bottom to the IP anomaly at Jeep Mine in the inversion model, consistent with the sulfide-bearing veins throughout 2,892 ft of drill core in NB26-003.