BMEX Gold Inc. discussed the visual results of the first two holes drilled into the geophysical anomaly on Dunlop Bay Ouest. Both holes have intersected massive sulphides. The first hole (BD-22-01) was drilled to test the interpreted plate below the known plate in the heart of the known Dunlop Bay Ouest showing. Hole BD-22-01 intersected a 7.00-metre (m) stringer (STR) zone composed of Pyrite (PY), Pyrrhotite (PO), trace Chalcopyrite (CP) and
trace Galena (GN) followed by semi-massive Pyrite-Pyrrhotite-1% Chalcopyrite over 1.00 m. This intersection extends the mineralization plan of the Dunlop Bay Ouest historical showing 100 m downdip. The second hole targeted a new plate and represents a new discovery of 3.85 m of massive sulfides composed of pyrrhotite, pyrite and traces of chalcopyrite and traces of sphalerite. BD-22-02; encountered one of the most conductive electromagnetic (EM) plates at Dunlop Bay Ouest. The massive sulfide lens from hole BD-22-02 overlies 3.60 m of massive magnetite (MT) itself overlying on a package of felsic rocks. A stringer zone of 5.85 m of Pyrite-Pyrrhotite-Magnetite and traces to 1% Chalcopyrite crosscutting the felsic unit was also observed underneath the massive magnetite. Hole BD-22-02 tested EM anomaly #2 on one related 1000 Siemens plate. The new discovery is 220 m north of historical hole ME-8, which returned 6.84 g/t Au over 1.50 m on the very edge of another 1000 Siemens plate.