Experimental Constraints on Type B CAI Formation: (1) fO2 Variations in Spinel Minor Element Partitioning, (2) Sub-Solidus Re-Equilibration Effects

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Our experimental results on an average type B CAI for spinel+liquid
field at a range of fO2 conditions we show that observed abundances of
Ti and V of spinels enclosed by fassaites may have been, at least in
part, produced by sub-solidus re-equilibration.

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