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Table 2 Average compositions of minerals from dyke-type rodingite and metagabbro

From: Interplay of irreversible reactions and deformation: a case of hydrofracturing in the rodingite–serpentinite system

 

Dyke-type rodingite131018-1B

Metagabbro 131019-MG

 

Di

Grt1a

Grt 2b

Chl

Di

Chl

Ttn

Ep

 

n c = 10

n = 7

n = 10

n = 6

n = 5

n = 3

n = 3

n = 13

SiO2

54.66

39.26

39.95

29.69

53.32

29.81

30.75

39.26

TiO2

0.15

38.47

Al2O3

1.18

18.04

21.49

21.18

2.01

20.25

1.19

29.10

Fe2O3

5.85

1.34

5.40

FeO

2.59

3.77

4.93

4.55

0.41

MnO

0.50

0.19

MgO

16.81

29.70

15.61

29.48

CaO

24.80

36.17

36.96

0.09

23.72

29.10

24.68

Na2O

0.44

Total

100.04

99.97

99.74

84.43

100.03

84.28

99.92

98.44

  

apfu

   

apfu

  

O

6

12

12

28

6

28

5

12.5

Si

1.98

3.01

3.01

5.76

1.95

5.82

1.00

3.02

Ti

0.01

0.95

Al

0.05

1.63

1.91

4.84

0.09

4.66

0.05

2.64

Fe3+

0.34

0.08

0.31

Fe2+

0.08

0.61

0.15

0.74

0.01

Mn

0.03

0.03

Mg

0.91

8.59

0.86

8.58

Ca

0.96

2.97

2.98

0.02

0.93

1.02

2.03

Na

0.03

Σcation

3.98

7.99

7.98

19.82

4.01

19.83

3.03

8.00

XMg

0.92

0.93

0.85

0.92

XSps

0.01

XGrs

0.82

0.96

XAdr

0.17

0.04

  1. aGrt1: Fe-rich garnet
  2. bGrt2: Fe-poor garnet
  3. cn: number of analyzed grains