PJX Resources Inc. announced that 3-dimensional modelling of airborne geophysical survey data has identified a strongly conductive MobileMT (MT) anomaly with a coincident magnetic (mag) signature that could be related to massive sulphide mineralization. The anomalies occur in a geological environment with potential to host a Sullivan type massive sulphide deposit at the Lewis Ridge target on PJX's Dewdney Trail Property near Cranbrook, British Columbia. Sullivan massive sulphide deposit contains iron sulphides with zinc, lead, silver and other metals that can be conductive and/or magnetic.

Modelling of airborne survey data by Expert Geophysics has defined a highly conductive MT anomaly at depth beneath Lewis Ridge and adjacent to the Jackleg fault. The Jackleg fault is considered to be the eastern extension of the Kimberley fault at the Sullivan deposit. Both faults were active during the Sullivan time.

The strongly conductive Lewis Ridge target can be traced for over 2.5km away from the Jackleg fault. For comparison, Sullivan deposit extends away from the Kimberley fault for 1 to 1.5km. Conductive core of the Lewis Ridge target occurs at depths ranging from 400 to 800 m, depending on topography.

Conductive core appears coincident with a magnetic anomaly. Anomalous gold, copper, zinc, lead, silver, arsenic, bismuth and/or molybdenum mineralization occur in soils with quartz veining along a 3 km trend on top of Lewis Ridge. Lewis Ridge soil anomalies occur along a major anticline fold axis and may be related to remobilized mineralization from a deposit at depth due to folding and faulting.

Mapping suggests the conductive and magnetic anomalies may occur at or below the Lower-Middle Aldridge Contact (LMC) which is the geological equivalent time for the Sullivan Deposit.