fig11.htm

Figure 12. Results of geochemical thermometry for the MZ rocks at P =1 kbar and 0.1 wt.% H2O in the starting compositions. Thin lines correspond to the equilibrium crystallization trajectories calculated at closed O2 conditions for seventeen Pl - Aug - Mt - Ilm - Pigpm Ol gabbros. The temperature of 1090 pm 5oC is assumed to indicate that intrinsic to the residual liquid (Table 3). Thick line represents calculations for the average MZ composition at QFM (see Figure 5).


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