Table T4. Equilibrium temperatures calculated by three different geothermometers, Hole 1256D.
Sample |
QUILF temperature (°C) |
Putirka temperature (°C) |
Ti-in-amphibole temperature (°C) |
|---|---|---|---|
| 335-1256D-235R-1W-19 | 940 ± 50 | 936 | 586* |
| 335-U1256D-Run12-RCJB-B | 994 ± 60 | 929 | 596*– 626† |
| 335-U1256D-Run12-RCJB-Q | 958 ± 62 | 981 | 853‡ |
| 335-U1256D-Run12-RCJB-S | 961 ± 53 | 967 | |
| 335-U1256D-Run15-EXJB | 962 ± 92 | 942 | |
| 335-U1256D-Run19-RCJB-D | 930 ± 44 | 974 | 509* |
* = overgrowth, † = average of different veins and clusters, ‡ = blebs in orthopyroxene. QUILF calculated according to Andersen et al. (1993) based on the two-pyroxene equilibrium. Putirka calculated according to Putirka (2008) based on the two-pyroxene equilibrium. Ti-in-amphibole temperature calculated according to Ernst and Liu (1998).
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