Major element compositions (wt%) of parental magmas modeled in this study using rhyolite-MELTS v.1.2.0.
. | Parental magmas . | |||
---|---|---|---|---|
Rock/Melt type1 . | Amphibolite (High-Al tholeiite) . | Leucoamphibolite (High-Mg andesite) . | Picrite2 . | Komatiite . |
SiO2 (wt%) | 47.71 | 52.27 | 46.16 | 46.61 |
TiO2 | 0.51 | 1.3 | 0.41 | 0.29 |
Al2O3 | 17.63 | 15.42 | 13.95 | 11.94 |
FeOt | 9.81 | 9.4 | 10.02 | - |
Fe2O3t | - | - | - | 11.94 |
MnO | 0.17 | 0.15 | 0.17 | 0.23 |
MgO | 9.36 | 6.94 | 17.45 | 28.06 |
CaO | 12.96 | 10.65 | 10.30 | 5.79 |
Na2O | 1.64 | 2.91 | 1.29 | 0.22 |
K2O | 0.14 | 0.51 | 0.11 | 0.45 |
P2O5 | 0.06 | 0.44 | 0.05 | 0.02 |
Cr2O3 | 0.06 | 0.05 | 0.06 | 0.352 |
NiO | 0.002 | 0.003 | 0.01 | 0.17 |
Mg#3 | 65 | 59 | 76 | 84 |
H2O4 | 0, 0.25, 2, 4 | 0, 0.25, 2, 4 | 0, 0.25, 2, 4 | 0, 0.25, 2, 4 |
. | Parental magmas . | |||
---|---|---|---|---|
Rock/Melt type1 . | Amphibolite (High-Al tholeiite) . | Leucoamphibolite (High-Mg andesite) . | Picrite2 . | Komatiite . |
SiO2 (wt%) | 47.71 | 52.27 | 46.16 | 46.61 |
TiO2 | 0.51 | 1.3 | 0.41 | 0.29 |
Al2O3 | 17.63 | 15.42 | 13.95 | 11.94 |
FeOt | 9.81 | 9.4 | 10.02 | - |
Fe2O3t | - | - | - | 11.94 |
MnO | 0.17 | 0.15 | 0.17 | 0.23 |
MgO | 9.36 | 6.94 | 17.45 | 28.06 |
CaO | 12.96 | 10.65 | 10.30 | 5.79 |
Na2O | 1.64 | 2.91 | 1.29 | 0.22 |
K2O | 0.14 | 0.51 | 0.11 | 0.45 |
P2O5 | 0.06 | 0.44 | 0.05 | 0.02 |
Cr2O3 | 0.06 | 0.05 | 0.06 | 0.352 |
NiO | 0.002 | 0.003 | 0.01 | 0.17 |
Mg#3 | 65 | 59 | 76 | 84 |
H2O4 | 0, 0.25, 2, 4 | 0, 0.25, 2, 4 | 0, 0.25, 2, 4 | 0, 0.25, 2, 4 |
1Source for parental compositions can be found in Supplementary Materials 6.
2Picrite estimated with PRIMELT3 based on High-Al tholeiite parental, following procedure for basalts of Herzberg & Asimow (2008, 2015).
3Mg# number is defined as molar Mg/(Mg + Fe2+)*100, Fe2+ is assumed to be 90% of total FeO unless Fe3+ has been estimated.
4Initial H2O contents in wt. %, compositions normalized to 100% in modeling.
Major element compositions (wt%) of parental magmas modeled in this study using rhyolite-MELTS v.1.2.0.
. | Parental magmas . | |||
---|---|---|---|---|
Rock/Melt type1 . | Amphibolite (High-Al tholeiite) . | Leucoamphibolite (High-Mg andesite) . | Picrite2 . | Komatiite . |
SiO2 (wt%) | 47.71 | 52.27 | 46.16 | 46.61 |
TiO2 | 0.51 | 1.3 | 0.41 | 0.29 |
Al2O3 | 17.63 | 15.42 | 13.95 | 11.94 |
FeOt | 9.81 | 9.4 | 10.02 | - |
Fe2O3t | - | - | - | 11.94 |
MnO | 0.17 | 0.15 | 0.17 | 0.23 |
MgO | 9.36 | 6.94 | 17.45 | 28.06 |
CaO | 12.96 | 10.65 | 10.30 | 5.79 |
Na2O | 1.64 | 2.91 | 1.29 | 0.22 |
K2O | 0.14 | 0.51 | 0.11 | 0.45 |
P2O5 | 0.06 | 0.44 | 0.05 | 0.02 |
Cr2O3 | 0.06 | 0.05 | 0.06 | 0.352 |
NiO | 0.002 | 0.003 | 0.01 | 0.17 |
Mg#3 | 65 | 59 | 76 | 84 |
H2O4 | 0, 0.25, 2, 4 | 0, 0.25, 2, 4 | 0, 0.25, 2, 4 | 0, 0.25, 2, 4 |
. | Parental magmas . | |||
---|---|---|---|---|
Rock/Melt type1 . | Amphibolite (High-Al tholeiite) . | Leucoamphibolite (High-Mg andesite) . | Picrite2 . | Komatiite . |
SiO2 (wt%) | 47.71 | 52.27 | 46.16 | 46.61 |
TiO2 | 0.51 | 1.3 | 0.41 | 0.29 |
Al2O3 | 17.63 | 15.42 | 13.95 | 11.94 |
FeOt | 9.81 | 9.4 | 10.02 | - |
Fe2O3t | - | - | - | 11.94 |
MnO | 0.17 | 0.15 | 0.17 | 0.23 |
MgO | 9.36 | 6.94 | 17.45 | 28.06 |
CaO | 12.96 | 10.65 | 10.30 | 5.79 |
Na2O | 1.64 | 2.91 | 1.29 | 0.22 |
K2O | 0.14 | 0.51 | 0.11 | 0.45 |
P2O5 | 0.06 | 0.44 | 0.05 | 0.02 |
Cr2O3 | 0.06 | 0.05 | 0.06 | 0.352 |
NiO | 0.002 | 0.003 | 0.01 | 0.17 |
Mg#3 | 65 | 59 | 76 | 84 |
H2O4 | 0, 0.25, 2, 4 | 0, 0.25, 2, 4 | 0, 0.25, 2, 4 | 0, 0.25, 2, 4 |
1Source for parental compositions can be found in Supplementary Materials 6.
2Picrite estimated with PRIMELT3 based on High-Al tholeiite parental, following procedure for basalts of Herzberg & Asimow (2008, 2015).
3Mg# number is defined as molar Mg/(Mg + Fe2+)*100, Fe2+ is assumed to be 90% of total FeO unless Fe3+ has been estimated.
4Initial H2O contents in wt. %, compositions normalized to 100% in modeling.
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