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

Figure 5

ATV structural analysis of drill hole S834. Disseminated mineralization occurs in a nongraphitic shear zone when it turns from NNE to NE and when dips decrease from highly steeply dipping to low angle dipping. The red arrow indicates the progressive decreasing in dip and the azimuth reorientation. Legend in Figure 2.