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Sakuramura Formation
- Coherent formation
- Pleistocene
- Lithofacies: Interbedded mudstone and sandstone
- Thickness: 500 - 700 m
- Upper limit: Unknown
- Lower limit: Conformity (Nagasawa Tuff Bed)
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Suzuka city, Mie pref.
- Hoshi et al. (2013) Jour. Geol. Soc. Japan, vol.119, no.10, pp.679-692 DOI