BMEX Gold Inc. announced an exploration update on a recently completed field program on the Dunlop Bay Property in the Abitibi region, Québec, Canada. The program is designed to: 1) validate presence and location of historical mineralization; 2) enhance the understanding of the various structural and geological controls to help design this fall's drilling program; 3) find the continuity of existing mineralization and; 4) discovery of new showings. Previous data compilation on Dunlop Bay showing had identified high grade surface gold mineralization including the Bella (historical grab samples returned up to 273.71 g/t Au, GM 16102) and Omela veins (historical grab samples returned up to 14.46 g/t Au, GM 16102).

To date, the team has identified and validated the location of most of the mineralization highlighted in the compilation of historical work including the Bella, Omela, Edith, Rollande, Venus and Galena veins. Several samples were taken on each mineralized zone and results are pending from ALS Laboratory. These veins are hosted along a WNW-trending corridor forming an approximately 2 km long highly prospective horizon for mineralization.

The summer field work suggests that the structures encountered continues Eastward of the Dunlop Bay showing with a possible untested link between Bella and Omala veins. Field reconnaissance made on Dunlop Bay West showing (or Ghislau) and on westward extension along the ground Electro Magnetic (EM) survey grid led to the identification of anomalously pyritized (10-25% pyrite and minor chalcopyrite) intermediate to felsic lavas located in the environment of the detected EM anomalies 1, 2 and 3. The historical Ghislau showing was found slightly south of EM Anomaly 3, and is composed of a 2 to 3 metres thick horizon oriented N300/65 of silicified intermediate to felsic rock overlaying between two flows of hyaloclastic to flow brecciated basalts. Orientation and dip of the anomalous pyrite-rich horizon show that it could be related with conductor Anomaly 3 at depth.

The Ghislau showing confirms the sulfides-rich mineralization style and the high potential of lateral continuity along the WSW trend provided by EM anomalies 1 and 2.