At the north end of the system (Doris North), the veins are folded into a doubly plunging anticline with the high-grade hinge zone lying close to the surface.
The Porky Lake deposit, located 3 km north of the Seabee mine (Figure 24), consists of shear zone hosted mineralization proximal to the hinge area of the regional Porky Lake anticline.
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The George Lake and Goose Lake gold deposits are hosted within units of banded iron formation within greywacke folded into an anticline, with the apex of the fold forming a hinge zone near surface.
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Gold mineralization is mainly hosted by sedimentary units of the Armina Formation, in the hinge and along the southern limb of a moderately southwest plunging anticline.
Within the hinge and along the south limb of the Boston-Richardson anticline, this zone has averaged 3.55 g/t over an average width of 16.59 metres from 18 of the 20 drill holes intersecting the zone over a 150 metre strike length.
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