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Wagakunisan Metamorphic Rocks Miyazaki et al., 1992
- Metamorphic facies (Cordierite isograd): 0.15 - 0.31 GPa, 400 - 580 degrees Celsius
- Lithofacies (Upper): Mélange facies
- Lithofacies (Middle): Coherent facies
- Lithofacies (Lower): Coherent facies
- Lithofacies (Protolith, Upper, Main): Mudstone, Mudstone-dominant interbedded sandstone and mudstone
- Lithofacies (Protolith, Upper, Minor): Chert, Limestone
- Lithofacies (Protolith, Middle): Sandstone, Sandstone-dominant interbedded sandstone and mudstone
- Lithofacies (Protolith, Lower): Mudstone, Mudstone-dominant interbedded sandstone and mudstone
- Lithofacies (Biotite zone): Biotite slate, Biotite schist
- Lithofacies (Cordierite zone): K-feldspar-cordierite-biotite schist, K-feldspar-cordierite-biotite hornfels
- Thickness (Apparent): 6,500 m or thicker
- Distribution: Dorokujin pass, Kasama city - Ishioka city, Ibaraki pref.; Yamazaki, Iwama, Kasama city, Ibaraki pref.; Mount Wagakunisan, Kasama city, Ibaraki pref.; Itajiki, Iwase, Sakuragawa city, Ibaraki pref.; Maie, Ishioka city, Ibaraki pref.; Amabikikannon temple, Motoki, Sakuragawa city, Ibaraki pref.
- Takahashi et al. (2011) Jour. Geol. Soc. Japan, vol.117, Supplement, pp.21-31 DOI
- Miyazaki et al. (1996) Geology of the Makabe District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 103p. (in Japanese with English abstract 4p.)