Geological map of the area around the Aldermac mine, showing location of old mine and the sulfide lens discovered in 1987 (after Hunter, 1979; and Deak Resources maps). The sulfides are hosted by a mafic to felsic volcanic sequence cut by probably synvolcanic sills of gabbro and quartz-feldspar porphyry. The Aldermac syenite truncates the northern part of the sequence.

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