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Fig. 13 | Swiss Journal of Geosciences

Fig. 13

From: Serpentinite dehydration at low pressures

Fig. 13

Mg#s of olivine vs. paragenetic phases from phase diagram section computation (using the 2002 revised data base of Holland and Powell (1998) augmented with Cr (Klemme et al. 2009) and corresponding solution models) are represented by the dashed fits and compared with the fits from this study. Partitioning between olivine and other phases was calculated for temperatures listed in Additional file 13: Table S8: Opx (750 and 800 °C), Anth (650, 675, 700 °C), Chl (500, 550, 600, 650, 675 and 700 °C), Ca-amphibole (500, 550, 600, 650, 675, 700, 750 and 800 °C) and Tc (550 and 600 °C)

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