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Inagawa Sandstone Member
- Coherent formation
- late Pliocene - early Pleistocene
- Sedimentary facies: Marine
- Sedimentary facies: Channel-fill deposit
- Lithofacies: Sandstone
- Paleocurrent: from North
- Thickness: 0 - 100 m or thicker
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Takada plain - Niigata plain, Niigata pref.
- Tanabe (2015) Jour. Geol. Soc. Japan, vol.121, no.9, pp.311-323, DOI
- Takano (2011) Jour. Geol. Soc. Japan, vol.117, no.4, pp.238-258 DOI
- Kobayashi et al. (2010) Jour. Geol. Soc. Japan, vol.116, no.11, pp.XVII-XVIII
- Kobayashi et al. (1993) Geology of the Izumozaki District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 91p. (in Japanese with English abstract 4p.)