Abstract
The distribution of Ba, Rb and Sr during crystallization of a granitic melt is examined in a number of theoretical models. The modes of crystallization considered are perfect fractional crystallization, perfect equilibrium crystallization, and an intermediate mode, incremental equilibrium crystallization. The effect of the degree of separation of cumulus minerals from melt during crystallization is also considered. Perfect fractional and incremental equilibrium crystallization (with small increments) are broadly similar, but differ in the final stages of crystallization in that the latter mode defines a finite trace element composition for the last solid. The effect of intercumulus melt in both modes of crystallization imparts a ‘liquid’ character to the solids, and suppresses the degree of enrichment of Rb and depletion of Ba and Sr in late solids and melts. Examination of trace element data for the Acid Phase of the Bushveld Igneous Complex in the light of these models suggests that these granites represent a suite of cumulate rocks, containing relatively large amounts of intercumulus melt.
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