Ref.: E. Takazawa et al. , Journal of Petrology, V 40, N 12, December 1999, pp. 1827-1851.
Type V layer : Gabbronorite mafic granulite layer.
These mafic layers (mm to m thickness scale) are parallel to foliation plane of the peridotites.
The assemblages are due to subsolidus reaction.
Mineral List:6 entries listed. 3 valid minerals.
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