fig10.htm

Figure 11. Results of geochemical thermometry for the LZc 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 nine Ol - Pl - Aug - Mt - Ilmpm Pig gabbros. The temperature of 1100 pm 5oC is assumed to be that intrinsic to the residual liquid (Table 3). Thick line represents calculations for the average LZc composition at QFM (see Figure 5).


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