The Survey identified a total of 94 km of primary northeast-southwest oriented structural corridors (Figure 1, black lines), occurring over 33 km strike length of the Property, that share similar geophysical characteristics to a number of Athabasca Basin high-grade uranium deposits (“uranium deposits”) (Figure 1). Specific characteristic details have been identified and are known to occur within other uranium deposits. These include the following:
- conductive zones exceeding 10 km in contiguous strike length (Figure 1, conductors 1 and 3),
- conductor offsets (“jogs”) associated with very conductive materials (“bright spots”) (Figure 1, Inset 3),
- jogs associated with the lack of conductive materials (“low spots”) (Figure 1, Inset 2), and
- bifurcated and sub-parallel conductors (Figure 1, Inset 1).
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