The Property
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History and Geological Background
The mineralization on the property is exposed on Beattie Island within Lac Duparquet and is hosted within the Destor Theolitic Unit of the Blake River Group. Mineralization is associated with interflow volcanic sediments between andesite flows and dioritic sills. The alteration consists of silicification, carbonization and considerable sulphide enrichment. Gold occurs with pyrite-chalcopyrite in shallow dipping quartz veins which crosscut the stratigraphy. Historical channel samples completed by Lacana Mining Corporation in 1982 include 0.81 oz/ton over 5 feet, 0.165 oz/ton over 6 feet and 0.10 oz/ton over 10 feet.
This property is located approximately 0.5 km directly to the west of the former Consolidated Beattie and Donchester gold Mines which produced over 1.0 million oz of gold between 1933-1956. The mineralization appears to be located in a splay off the Porcupine Destor Fault Zone.



