All three drill holes completed to date on the New Extension Target have returned significant intervals of sulphide mineralization up to 135 meters. They consist of stringers and aggregations of semi-massive to massive pyrrhotite, chalcopyrite and pyrite within veins, stockwork and breccia. Sulphide mineralization has been observed throughout the drill holes and remains open.
The type of mineralization (including semi-massive to massive pyrrhotite and pyrite), textures (including veining, stockwork and brecciation) and alteration (chloritization, silicification, epidotization) observed in the New Extension Target located in the underlying volcanics are similar to what has been observed in drill holes and at surface on the
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