PJX Resources Inc. announced recently received results of significant zinc and lead mineralization in outcrop that further supports the potential to discover a Sullivan type deposit on the Company's Dewdney Trail Property in the Sullivan Mining District in southeastern British Columbia, Canada. Two rock samples taken from outcrop, G23-699B and G23-699C below, returned values of 5.57% zinc, 0.94% (9450ppm) lead, 4.41g/t (4.41ppm) silver, and 4.72% zinc, 1.28% lead, 6.07g/t (6.07ppm) silver, respectively. The sediment hosted zinc and lead mineralization appears as bands or beds.

The bedrock exposures of mineralization occur upslope and north of semi-massive to massive sulphide boulders containing Sullivan deposit style and grade mineralization announced in the news release dated October 12, 2023. Semi-massive to massive sulphide boulderers occur in talus at the base of the mountain slope. Outcrop with sediment hosted zinc-lead-silver mineralization occurs up-slope and to the north of the boulders' location.

(photo looking northeast); The strongly magnetic semi-massive to massive sulphides boulders occur at the base of the mountain slopes and on the edge of a large (about 500m diameter) strong magnetic geophysical anomaly (pink to red coulours on the airborne magnetic map) that occurs upslope from the boulders; Zinc-lead-silver sulphide mineralization in outcrop is only very weakly magnetic. This supports the potential for a vertically or laterally zoned deposit with varying magnetic signatures. The outcrop mineralization appears to be associated with a less magnetic trend (orange to red coulours) in the airborne geophysics survey that occurs for possibly 1.6 km along strike.