No economic base metal sulphide mineralization was intersected in the drilling program. The extension of the two previously drilled holes has provided a more complete cross-section of the Waconichi Formation. Although anomaleous Cu and Zn mineralization is present in the holes, no priority targets are defined in the vicinity of the holes at this time. The source of the DeepEMconductor and associated MaxMin anomaly located near the contact of the Border Zone of the Dore Lake Complex and felsic volcanics appears typical of the stringer style sulphides associated with the Dore Lake Complex. It is not thought to be of potential economic significance. Although significant hydrothermal alteration and anomaleous zinc mineralization are present in the felsic volcanic rocks of hole L00-02, no conductive sulphide mineralization was identified within the range of the Pulse EM survey.
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