High-pressure granulite facies
Chemical Process (Solid-phase growth) - Middle-P metamorphic facies series
Index Minerals
Sapphirine, Osumilite
Required Geological Setting
Accretionary complexes + Middle-P metamorphic rocks
Occurrence
Metamorphic rocks formed by regional metamorphism in the following condition: more than 700 degree and 1.0-1.5 GPa (30-50 km depth). A metamorphic facies formed in subduction zones. High-pressure granulite facies metamorphic rocks are in Barrovian-type middle-P metamorphic rocks.
Change of mineral assemblages
- [ Extinct ] Garnet, Cordierite
- [ Appear ] Sapphirine, Osumilite
Mineral Assemblages
- [ Felsic Rocks ] Quartz, Plagioclase, K-feldspar, (Hornblende, Biotite)
- [ Mafic Rocks ] Clinopyroxene (Diopside), Plagioclase, (Orthopyroxene (Hypersthene))
- [ Ultramafic Rocks ]
- [ Mudstone ] Sapphirine, Orthopyroxene (Hypersthene), Sillimanite, K-feldspar, Quartz, (Osumilite)
- [ Laterite ]
- [ Bedded Mn ]
- [ Carbonate Rocks ]