fig08.htm

Figure 8. Results of geochemical thermometry for the LZa 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 six Ol - Pl gabbros. The temperature of 1145 pm 5oC is assumed to indicate that intrinsic to the residual liquid (Table 3). Thick line represents calculations for the average LZa composition at QFM (see Figure 5). Two dashed lines belong to the samples LA-347 and LA-753 are excluded from further considerations.


This document was generated by TeXWeb (Win32, v.1.3) on February 3, 2003.