Renforth’s wholly owned Malartic Metals Package property hosts the Beaupré copper/silver discovery, traced over ~160m and partially stripped to uncover copper and silver within quartz veining, oriented SW to NE within <2km of the Cadillac Break.
Beaupré Regional Setting
Beaupré Local Setting
A northeast-striking deformation zone, hosted by near-massive sedimentary units, can be traced over about 160 m along a ridge crest in the north of the property. It has a southwest dip of ~55°. At its narrowest (~20 cm) it has the appearance of a weakly chloritized shear zone. In places it widens to form a ~1 m thick zone of silicification, brecciation and quartz flooding. Very coarse, irregular clots of chalcopyrite as well as tight disseminations of fine pyrite are emplaced within the vein and along the immediate margins. Samples return elevated Cu and Ag from this material. The depth and strike extensions are yet to be determined, and it is not clear if parallel vein sets are present.
