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Shashakiyama Formation Sato et al., 2022
- Type locality: Mount Shinjoyama - Mount Shashakiyama, Okayama city, Okayama prefecture
- Volcanic rocks
- Late Cretaceous (ca. 95.2 Ma, FT)
- Intruded by: Momoezuki Quartz Diorite
- Sedimentary facies: Terrestrial
- Sedimentary facies (Minor): Lacustrine
- Lithofacies (Top): Biotite hornblende rhyolite welded tuff
- Lithofacies (Upper): Dacite - Rhyolite lapilli tuff, Tuff
- Lithofacies (Middle): Hornblende-bearing biotite rhyolite welded tuff, Lapilli tuff
- Lithofacies (Lower): Rhyolite tuff, Mudstone
- Lithofacies (Bottom): Biotite rhyolite tuff, Lapilli tuff
- Thickness: 700 m or thicker
- Thickness (Top): 120 m or thicker
- Thickness (Upper): ca. 150 m
- Thickness (Middle): 200 m or thicker
- Thickness (Lower): Several - 30 m
- Thickness (Bottom): ca. 200 m
- Distribution (East - West): 5.6 km
- Distribution (South - North): 5.2 km
- Upper limit: Unconformity (Takasagoyama Formation, Kibi Group)
- Lower limit: Unconformity (Ejiri Unit)
- Distribution: Mount Shinjoyama - Mount Shashakiyama - Mount Ohibatayama, Okayama city, Okayama pref.
- Sato et al. (2022) Geology of the Wake District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, AIST, 106p. (in Japanese with English abstract 4p.)