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Table 2 Distribution of U, Th, and K for the different alteration zones through drift# DI and D#II at El-Missikat exploratory tunnels

From: 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, Egypt

Lithology/alterations

U (ppm)

Th (ppm)

K (%)

Th/U

(Th/K)*10–4

(U/K)*10–4

DI

 Brecciation

Avg., 43.32

58.93

4.57

1.4

15.19

11.17

Max., 69.2

71.6

7.3

2.29

49

37

Min., 29.2

48.2

1.2

0.76

7.65

4.29

 Silicification

Avg., 41.63

63.67

3.12

1.57

23.1

15.61

Max., 59.1

71.9

6.7

2

31.38

26.86

Min., 33.8

56.4

1.9

0.95

10.57

5.28

 Greisenization

Avg., 41.77

57.32

4.48

1.45

13.82

10.08

Max., 71.9

72.5

6

2.46

38.33

23.33

Min., 26.4

44.5

1.5

0.78

8.56

4.56

 Kaolinization

Avg., 29.73

56.21

4.15

1.93

14.34

7.44

Max., 37.2

63.5

5.7

2.79

19.9

10.78

Min., 22.1

49.2

2.7

1.48

8.63

5.14

DII

 Brecciation

Avg., 41.53

61.72

6.12

1.5

10.15

6.86

Max., 45.0

72

7.6

1.79

12.82

8.42

Min., 36.20

45.6

5.3

1.01

7.35

5.04

 Greisenization

Avg., 36.11

56.4

4.46

1.64

14.34

9.38

Max., 95.6

70.2

6.9

3.03

89.86

65

Min., 19.0

36.3

0.7

0.6

8.05

4.45

 Kaolinization

Avg., 29.84

54.89

4.9

1.87

11.57

6.32

Max., 37.2

63

6.1

2.72

17.11

10.69

Min., 23.2

45.4

3.2

1.4

8.05

4.62