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Oyama Formation Takimoto, 1935
- Type locality: Oyama, Ichishi town, Tsu city, Mie prefecture
- Coherent formation
- Pliocene
- Sedimentary facies: Alluvial fan deposit at the front of Nunobiki mountains
- Lithofacies: Gravels
- Lithofacies (Minor): Sands, Silt, Clay
- Sedimentary structures: Parallel stratification, Imbricate structure
- Paleocurrent: from North to South
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Oyama, Ichishi town, Tsu city, Mie pref.; Katada - Lake Sakuraike, Katada town, Tsu city, Mie pref.; Shibukuro town, Tsu city, Mie pref.; Suzuka city, Mie pref.
- Hoshi et al. (2013) Jour. Geol. Soc. Japan, vol.119, no.10, pp.679-692 DOI
- Yoshida et al. (1995) Geology of the Tsu-Seibu District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 136p. (in Japanese with English abstract 6p.)
- Yoshida et al. (1991) Geology of the Kuwana District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 154p. (in Japanese with English abstract 5p.)
- Yoshida (1984) Geology of the Yokkaichi District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 81p. (in Japanese with English abstract 5p.)