Fig. 9From: 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, EgyptBinary plot of Th vs. U through the different alteration zones at El-Missikat drifts# DI a, c, e, and f assigned to brecciation, greisenization, silicification, and kaolinization) and DII (b, d, and g assigned to brecciation, greisenization, and kaolinization) showing weak correlation coefficients as an indication for U-enrichmentBack to article page