Fig. 6From: Genetic implications of Th/U, Th/K, and U/K ratios for U mineralizations: A case study from El-Missikat and El-Erediya shear zones, Eastern Desert, EgyptField photographs show the occurrence of yellowish-greenish yellow secondary U minerals, at DI of El-Missikat shear zone, as fracture infill hosted by the brecciated silica veins a and associated with fluorite (b-look at red arrow), with occasional occurrence through the kaolinized granite (c)Back to article page