Fig. 10From: 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-Erediya drifts# DII a, c, and e assigned to brecciation, kaolinization, and hematitization) and DIII b, d, and f assigned to the same order) showing weak correlation coefficients as an indication for U-enrichmentBack to article page