Ref.: E. Takazawa et al. , Journal of Petrology, V 40, N 12, December 1999, pp. 1827-1851.
Type I layer : Al-Ti augite mafic gabbroic granulites (garnet clinopyroxenites) from cumulates of shallow depth formation (age : 80 Ma).
These mafic layers (mm to m thickness scale) are parallel to foliation plane of the peridotites.
The assemblages are due to subsolidus reaction.
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