Resistivity profile extracted from the 3D block model for Line 6200 (location in Figure 1). The east-west profile spans 1.2 km. The syenite breccia phase cemented by specularite at Iron Chief (see Photo 2 below) is immediately to the east of the conductor. Workings at the historic 1936 mine on the east flank of the Copper Queen hill and located immediately to the west of the conductor follow qz veins with copper sulfide associated with latite porphyry dykes in sodic diorite with pervasive secondary albite and hematite alteration.
Resistivity profile extracted from the 3D block model for Line 6200 (location in Figure 1). The east-west profile spans 1.2 km. The syenite breccia phase cemented by specularite at Iron Chief (see Photo 2 below) is immediately to the east of the conductor. Workings at the historic 1936 mine on the east flank of the Copper Queen hill and located immediately to the west of the conductor follow qz veins with copper sulfide associated with latite porphyry dykes in sodic diorite with pervasive secondary albite and hematite alteration.