Ref.: T. Morishita and S. Arai, Journal of Petrology, 2001, V 42, N 7, pp. 1279-1299.
Mafic layer in peridotite.
Corundum-bearing type II mafic HP gabbroic-troctolitic rock (mantle residue : olivine-plagioclase-clinopyroxene cumulate / P< 1.0 GPa).
Corundum : P > 1.5 GPa (posterior to cumulate formation).
5 entries listed. 4 valid minerals.
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