However, Proterozoic Pielavesi granulites of central Finland, which are accompanied by hypersthene granitoids, were formed at 800[degrees]C and 5-6 kbar and show evidence for near-isobaric cooling (Holtta 1988).
CIPW norms contain hypersthene (rocks are subalkaline; assuming [Fe.sub.2][O.sub.3]/FeO = 0.18; Irvine and Baragar 1971) which is consistent with tholeiitic Nb/Y ratios of ~0.3 and Ti[O.sub.2] concentrations (~1.3 wt.
The presence of hypersthene and corundum in the norm indicates a high [Al.sub.2][O.sub.3] content in the magma, which is also recognised in the rock analyses ([Al.sub.2][O.sub.3] 14.33-14.74 wt.
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