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Location: 0.1 km N from Balmertown, Ontario, Canada
17 Mine RoadBag 2000BalmertownOntario, CanadaP0V 1C0
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exes (Red Lake, Campbell and Cochenour) and the recently acquired Bateman Gold Project.Red Lake mineralisation is hosted in the Red Lake greenstone belt. Mineralisation is associated with multiple episodes of volcanism, sedimentation, plutonism and deformation and is hosted in a variety of rock types within the Red Lake Greenstone belt. Economic zones of mineralisation are characterised by vein hosted gold systems accompanying sulphide replacement within sheared mafic to komatiitic basalts. The Red Lake/Campbell, Cochenour, HG Young and McFinley deposits are hosted within significantly folded and sheared portions of the Balmer Assemblage dominated by tholeiitic basalt and komatiitic basalt intruded by felsic, mafic and lamprophyric intrusive rocks. Shear zones act as primary hydrothermal fluid corridors and host significant portions of the gold mineralisation in the area. Other significant mineralised structures occur within lower-strain areas of the stratigraphy. Orebodies
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Wade Warren