Iron in plagioclase as a monitor of the differentiation of the Skaergaard intrusion

Several recent publications suggest that the appearance of Fe-Ti oxides terminates iron enrichment and starts pronounced silica enrichment (the Bowen trend) during the differentiation of tholeiitic basalt. However, this does not appear to hold for the Skaergaard intrusion. New data from a similar to 950 m long drill core (90-22) through its Upper Zone reveal that: (1) iron in plagioclase increases from similar to 0.25 to similar to 0.45 wt% FeOT with fractionation of evolved oxide ferrodiorites (An(46-32)) and (2) the evolving liquid, which is modelled by incremental bulk-rock summation, increased its iron content from 20.1 to 26.5 wt% FeOT and its silica content from 47.4 to 49.6 wt% SiO2 with fractional crystallisation (the Fenner trend). Positive correlation between modelled iron-content of the magmas, and measured iron-content of plagioclase, confirms that iron enrichment is petrologically feasible even with Fe-Ti oxides in the fractionating assemblage. As suggested by previous authors, fractional crystallisation closed to oxygen exchange is the likely reason why some layered intrusions diverge from the Bowen mechanism of differentiation. It is emphasised that both trends seem to exist in nature.