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Table 3 Distribution of U, Th, and K for the different alteration zones through drift# DII and D#III at El-Erediya 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

DII

 Brecciation

Avg., 121.4

32

6.01

0.35

5.38

21.49

Max., 161.3

32.8

7.3

0.65

6.39

31.63

Min., 47.2

30.6

5.1

0.2

4.19

6.47

Hematitization

Avg., 110.84

33.24

6.91

0.37

4.85

16.14

Max., 266.1

41.8

8.2

0.67

6.47

32.45

Min., 49.7

26.6

5.9

0.13

3.8

6.37

Kaolinization

Avg., 35.79

35.69

6.78

1.12

5.83

5.71

Max., 89.2

102.5

8.3

2.91

51.25

29.7

Min., 12.9

26.5

2

0.34

3.61

1.7

DIII

 Brecciation

Avg., 116.54

39.44

6.56

0.38

6.04

17.78

Max., 184.6

58.7

7.2

0.56

8.27

26.75

Min., 61.6

29.3

5.3

0.16

4.25

9.78

 Hematitization

Avg., 124.01

35.46

6.29

0.3

5.76

20.04

Max., 184.6

43.8

7.1

0.42

7.08

26.75

Min., 66.0

23.2

4.8

0.16

3.27

9.3

 Kaolinization

Avg., 49.54

42.17

4.67

0.9

12.39

13.48

Max., 95.8

219.5

8.5

7.42

199.5

41.14

Min., 19.3

16.3

0.8

0.38

3.88

2.74