(UUID : b340e204-1229-4447-b9ae-92679b33c93b)
Rock
Biotite-sillimanite gneiss
M-063
Rock
metamorphic rock
It was metamorphosed at medium to high temperatures and has a higher degree of metamorphism than schist. The gneiss structure is developed. Recrystallization is evident. The foliation is less distinct than that of phyllite. Biotite and sillimanite are characteristic.
17.0
cm
Biotite, Plagioclase, Quartz, Epidote, Tourmaline
#metamorphic rock
Department of Geology and Geophysics, Kangwon National University
+82-33-250-8550
Igneous Petrology and Ladoratory
DOI
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The copyright of this data is held by KIGAM.
2024-09-04