52: Whole rock and modal compositions * (super a) Mg-# assumes all iron as FeO. Major element and V, Cr, Co, Ni, Sr and Ba abundances analyzed by ICP at Indiana University. Analyst: James Brophy. Estimated errors (1sigma, relative %) are: Si (<1), Ti (<0.5), Al (<1), Fe (<0.5), Mn (<2), Mg (<0.5), Ca (<0.5), Na (<2), K (<1.5), P (<10), V (<4), Cr (30), Co (<2), Ni (<15), Rb (<3), Sr (<2.5), Zr (<2.5), and Ba (<2). *

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53: Representative plagioclase core compositions

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54: Representative olivine core compositions * (super a) Whole rock FeO contents recalculated (Sack et al. 1980) for T-fo2 conditions of 1,110 C and NNO+0.6 log units *

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55: Representative clinopyroxene core compositions

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56: Representative titanomagnetic core compositions

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57: HAB and tholeiite compositions referred to in this study

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58: log (fO2/(fO2)NNO) T=1,110 degrees C

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59: Olivine tholeiite fractionation calculations

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60: Trace element distribution coefficients

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61: Summary of quartz eclogite modeling

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