0 a type of rock that breaks easily into thin layers, formed of mica or other minerals -- 片岩（容易裂成薄層的一種岩石，由雲母或其他礦物質構成）
A method for calculating effective bulk composition modification due to crystal fractionation in garnet-bearing schist: implications for isopleth thermobarometry.
The lower part of the formation is often metamorphosed and deformed into strongly magnetic mica schists.
The magnetization in the schist and the sandstone is interpreted to be a chemical remanant magnetization caused by the same fluids that precipitated the veins.
Metasedimentary samples from the southeastern portion are represented by graphite schist and metapelite.
The most common type is garnet-biotite schist consisting of biotite, garnet, feldspar and accessory zircon.
The schist is composed mainly of biotite, plagioclase and quartz, whereas granulitite consists mainly of quartz, plagioclase and biotite.
In schist intercalations within the marbles mineral assemblages include chlorite, calcite, albite, phengite and quartz.
The soils are well drained and derived from schist.
