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Takikubo Formation
- Type locality: Takikubo, Higashimiyoshi city, Miyoshi county, Tokushima prefecture
- Coherent formation
- Izumi sedimentary basin
- Forearc basin associated with strike-slip fault related to Median Tectonic Line
- Late Cretaceous
- Interfingered: Hiketa Formation, Shiroyama Formation
- Lithofacies: Interbedded sanstone and mudstone, Felsic tuff
- Sedimentary structures: Graded bedding, Sole marks, Slump structure
- Paleocurrent: from Northeast to Southwest
- Paleocurrent (Minor): from Northwest to Southeast
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Takikubo, Higashimiyoshi city, Miyoshi county, Tokushima pref.
- Noda et al. (2017) Geology of the Kan-onji District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, AIST, 96p. (in Japanese with English abstract 4p.)
- Kikuchi and Kotake (2013) Jour. Geol. Soc. Japan, vol.119, no.9, pp.613-629 DOI