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Table 5 EDX analysis of the separated radioactive minerals from some altered granites and silica veins at El-Missikat and 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

Elements %

Thorite

Betafite

Zircon

Coffinite

Uranophane

Kasolite

A

B

C

D

E

F

G

H

I

J

K

SiO2

34.82

28.30

–

–

45.9

42.2

25.2

23.8

38.9

53.92

43.88

UO2

8.55

10.90

36.9

28.7

4.2

3.4

65.8

67.2

53.7

33.73

30.03

ThO2

42.29

49.12

1.22

2.4

1.07

1.3

–

–

–

–

–

Al2O3

2.77

1.97

5.77

3.45

7.30

6.2

0.65

0.12

3.67

5.08

4.8

TiO2

–

–

25.5

29.2

–

–

–

–

–

–

–

CaO

–

0.42

1.4

1.08

1.95

2.7

1.2

2.5

1.0

1.97

–

PbO

–

0.30

–

0.10

–

–

2.3

2.51

0.1

0.2

20.17

FeO

2.98

0.25

2.35

2.16

1.58

–

0.9

1.7

1.5

4.32

–

BaO

–

–

0.08

0.48

–

–

0.5

0.9

–

–

–

ZrO2

–

–

–

–

30.9

35.5

–

–

0.1

0.4

–

Nd2O3

–

–

2.5

3.7

–

–

0.14

0.11

–

–

–

Y2O3

7.59

8.23

0.89

0.45

5.78

6.0

1.05

0.83

–

–

–

Ce2O3

–

–

1.53

2.78

–

–

0.29

0.28

–

–

–

Ta2O5

–

–

3.41

4.51

–

–

–

–

–

–

–

Nb2O5

–

–

16.6

20.7

–

–

–

–

–

–

–

Total

99.0

99.49

98.2

99.7

98.6

97.3

98.03

99.9

98.97

99.62

98.88

  1. *A—Greisenization through DII of El-Missikat; B—Kaolinization through DIII of El-Erediyal; C—red silica veins through DII of El-Erediya; D—brecciated silica veins through DI of El-Missikat; E—silicification through DI of El-Missikat; F—brecciated granite through DII of El-Erediya; G and H—massive and brecciated silica veins, respectively, through DII of El-Missikat; I and J—hematitization and red silica veins, respectively, through DIII of El-Erediya; K—brecciated silica veins through DII of El-Missikat