Stelmine Canada announced the discovery on its Courcy property of new gold values provided by rock samples (grab and channel) and of gold anomalies revealed by till samples. The Courcy property, located within an Archean greenstone belt at the western end of the metasedimentary Opinaca basin presents two types of gold mineralization: a stratiform type associated with a package of garnet-bearing amphibolites and sulphide-rich iron formations along a major refolded thrust fault (Couteau fault) extending more than 21 km (zones 1 and 2); second generation quartz veins invading the sheared contact of volcanic and sedimentary assemblages along the axis of a major fold (zone 4). New exploration work has supported the extension of zones 1 and 2 and the increased potential of zone 4. In addition to better helping to locate the location of drillholes for a future campaign, the work delineated the different sites associated with two mineralization types. Gold concentrations of 4.0 g/t from a 1.3 m channel and a grab sample value of 0.5 g/t Au were obtained from zone 4. Coupled with the results of the till survey showing a significant gold anomaly south of strongly folded and mylonitized rocks concealing a type 2 mineralization, these discoveries enhance the possibility of defining a mineralization extending more than 800 m. A gold value of 0.78 g/t on 1.1 m confirms the extension of zone 1 by more than 50 m toward the southwest. This type 1 mineralized projection is still open since it is buried under the till cover. Furthermore, the results of basal till samples revealed three northeast/southwest-oriented gold anomalous regions than can be traced upward the glacial transport to mineralized zones 1 and 2. Also note two anomalous sectors near the southern and southwestern contact of the Couteau fault which shows a similar folded structure to that associated with zones 1 and 2. The former areas expose little outcrop and warrant a re-evaluation with different exploration methods. A compilation of exploration work completed by Stelmine along the Couteau fault near the core of the antiform (including grab and channel samples, overburden stripping, geological, geophysical and structural surveys and till sampling) demonstrates a significant gold mineralization ready to be drilled.