Table 2

Overview of initial liquidus plagioclase composition in molar An(%) for each MELTS model presented in this study at various lithostatic pressure, initial water content and redox condition. Missing values are either due to instability of MELTS at high water contents at low pressure (1–2 kbar) or the replacement of plagioclase with garnet at high pressure (≥6 kbar).

  High-Al TholeiiteHigh-Mg AndesitePicriteKomatiite
H2O (wt %)P (kbar)-1dQFM+1-1dQFM+1-1dQFM+1-1dQFM+1
1868686717172858585888888
2858586697071858585888888
3858585696969848484888887
04848484686868848383888785
6838383666565848380877775
8828282636362797671615659
108181806160596763623840
1878787727373878787898989
2868687717172868686898989
3858686707070858585898988
0.254858585696969858585898987
6848484676666848380838182
88383826464638075686872
1082817962615965575456
1919191818181929292939392
2919190798078929289949493
3909088787976919187949393
24908786777974898784929392
68583827271698480789091
8827977676562787488
1078777557555571636184
2939392858483949293
3939288838180939390949493
44909087807576929087939493
6878583707268878380899292
878797863616382807491
107374755355597174
  High-Al TholeiiteHigh-Mg AndesitePicriteKomatiite
H2O (wt %)P (kbar)-1dQFM+1-1dQFM+1-1dQFM+1-1dQFM+1
1868686717172858585888888
2858586697071858585888888
3858585696969848484888887
04848484686868848383888785
6838383666565848380877775
8828282636362797671615659
108181806160596763623840
1878787727373878787898989
2868687717172868686898989
3858686707070858585898988
0.254858585696969858585898987
6848484676666848380838182
88383826464638075686872
1082817962615965575456
1919191818181929292939392
2919190798078929289949493
3909088787976919187949393
24908786777974898784929392
68583827271698480789091
8827977676562787488
1078777557555571636184
2939392858483949293
3939288838180939390949493
44909087807576929087939493
6878583707268878380899292
878797863616382807491
107374755355597174
Table 2

Overview of initial liquidus plagioclase composition in molar An(%) for each MELTS model presented in this study at various lithostatic pressure, initial water content and redox condition. Missing values are either due to instability of MELTS at high water contents at low pressure (1–2 kbar) or the replacement of plagioclase with garnet at high pressure (≥6 kbar).

  High-Al TholeiiteHigh-Mg AndesitePicriteKomatiite
H2O (wt %)P (kbar)-1dQFM+1-1dQFM+1-1dQFM+1-1dQFM+1
1868686717172858585888888
2858586697071858585888888
3858585696969848484888887
04848484686868848383888785
6838383666565848380877775
8828282636362797671615659
108181806160596763623840
1878787727373878787898989
2868687717172868686898989
3858686707070858585898988
0.254858585696969858585898987
6848484676666848380838182
88383826464638075686872
1082817962615965575456
1919191818181929292939392
2919190798078929289949493
3909088787976919187949393
24908786777974898784929392
68583827271698480789091
8827977676562787488
1078777557555571636184
2939392858483949293
3939288838180939390949493
44909087807576929087939493
6878583707268878380899292
878797863616382807491
107374755355597174
  High-Al TholeiiteHigh-Mg AndesitePicriteKomatiite
H2O (wt %)P (kbar)-1dQFM+1-1dQFM+1-1dQFM+1-1dQFM+1
1868686717172858585888888
2858586697071858585888888
3858585696969848484888887
04848484686868848383888785
6838383666565848380877775
8828282636362797671615659
108181806160596763623840
1878787727373878787898989
2868687717172868686898989
3858686707070858585898988
0.254858585696969858585898987
6848484676666848380838182
88383826464638075686872
1082817962615965575456
1919191818181929292939392
2919190798078929289949493
3909088787976919187949393
24908786777974898784929392
68583827271698480789091
8827977676562787488
1078777557555571636184
2939392858483949293
3939288838180939390949493
44909087807576929087939493
6878583707268878380899292
878797863616382807491
107374755355597174
Close
This Feature Is Available To Subscribers Only

Sign In or Create an Account

Close

This PDF is available to Subscribers Only

View Article Abstract & Purchase Options

For full access to this pdf, sign in to an existing account, or purchase an annual subscription.

Close