Inverted Chargeability data at a depth of 50 m in the Trojan – Condor Corridor. Surface showings identified by the previous operator are indicated. A circular magnetic feature is outlined by the white dashed line. The dark pink features evident on the underlying geology map are Triassic age diorite intrusions mapped at surface, spatially associated with the 3D IP geophysical anomalies, hosted by Nicola Group host rocks (green). These rocks were subsequently overlain by the Princeton Group (yellow), which cover the rocks of interest underlying the east side of the survey area.
Inverted Chargeability data at a depth of 50 m in the Trojan – Condor Corridor. Surface showings identified by the previous operator are indicated. A circular magnetic feature is outlined by the white dashed line. The dark pink features evident on the underlying geology map are Triassic age diorite intrusions mapped at surface, spatially associated with the 3D IP geophysical anomalies, hosted by Nicola Group host rocks (green). These rocks were subsequently overlain by the Princeton Group (yellow), which cover the rocks of interest underlying the east side of the survey area.