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Yatsugamaruyama Formation Itihara et al., 1986
It is considered as a part of Mino Belt
- Type locality: Mount Yatsugamaruyama, Izumi city, Osaka prefecture
- Accretionary complex
- Jurassic
- Intruded by: Quartz porphyry
- Sedimentary facies: Marine
- Lithofacies: Mudstone, Sandstone
- Lithofacies (Minor): Basalt lava
- Sedimentary structures: Foliation
- Distribution (East - West): ca. 500 m
- Distribution (South - North): ca. 500 m
- Upper limit: Unconformity? (Ogawa Andesite)
- Tamba Belt (Kishiwada, Osaka pref.)
- [ Upper ]
- /--/--/--/--/-
- Yatsugamaruyama Formation
- /--/--/--/--/-
- [ Lower ]
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Mount Yatsugamaruyama, Izumi city, Osaka pref.; Kogigawa river, Kaizuka city, Osaka pref.
- Itihara et al. (1986) Geology of the Kishiwada District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 148p. (in Japanese with English abstract 7p.)