Table 1 fO2 results for the Norwegian orogenic peridotites considered in this study. The P, T and Fe3+/Fetot used for fO2 calculation are also reported.

From: Garnet peridotites reveal spatial and temporal changes in the oxidation potential of subduction

Sample

Grt spot

Spectrum n°

Fe3+/Fetot

P (Gpa)

T (C°)

fO2 (ΔlogFMQ)

fO2 (ΔlogAPM)

GSD07_1

core

88

0.038

3.5

850

−0.9

1.7

GSD07_2

core

89

0.033

3.5

850

−1.2

1.4

GSD07_3

core

90

0.034

3.5

850

−1.2

1.4

GSD07_4

core

91

0.051

3.5

850

−0.5

2.1

GSD07_5

core

92

0.046

3.5

850

−0.6

2.0

GSD08_1

core

100

0.042

3.5

850

−1.0

1.6

GSD08_2

core

101

0.036

3.5

850

−0.8

1.8

GSD08_3

core

102

0.044

3.5

850

−0.7

1.8

GSD08_4

core

103

0.042

3.5

850

−0.7

1.9

GSD08_5

core

104

0.039

3.5

850

−0.9

1.7

GSD08_6

core

106

0.054

3.5

850

−0.4

2.2

BDN03_1*

rim

124

0.039

6.3

1000

−3.5

0.2

BDN03_2*

core

125

0.049

6.3

1000

−3.2

0.5

BDN03_3*

core

126

0.046

6.3

1000

−3.2

0.4

BDN02_1

corona

110

0.018

3.0

800

−1.0

1.4

BDN02_2

vein

111

0.030

3.0

800

−1.1

1.3

BDN02_3

exolution

112

0.021

3.0

800

−0.5

1.8

UGL01_1*

core

97

0.014

7.6

1573

−6.4

−2.4

UGL01_2*

core

98

0.038

7.6

1573

−4.8

−0.8

UGL01_3*

rim

99

0.033

7.6

1573

−4.9

−0.9

UGL03_2

vein core

115

0.018

7.4

1539

−5.0

−1.1

UGL03_3

vein core

116

0.058

7.4

1539

−3.5

0.5

SVT06_1

core

93

0.081

5.5

800

−1.9

2.5

SVT06_2

core

94

0.095

5.5

800

−1.7

2.7

SVT06_3

transition

95

0.078

5.5

800

−2.1

2.3

SVT06_4

pyroxenite

96

0.089

5.5

800

−1.8

2.6

  1. Samples with asterisk are from ref.13.