Structural Controls of Uranium Mineralization in the Basement of the Athabasca Basin, Saskatchewan, Canada

Figure 21

Sketch representing the reactivation of shear zones and the formation of dilational jogs and conjugated faults depending on their orientation respect to a NNE σ1: reverse left-lateral in Spitfire, reverse right-lateral in Sue, and conjugated in Tri-Island. Mineralization is in pink.