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 |