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Hiwasa Formation
- Accretionary complex
- Deposition: Late Cretaceous, Campanian - Maastrichtian (Radiolarians)
- Deposition: Late Cretaceous, Maastrichtian - Paleogene (71.3 - 67.8 Ma, U-Pb)
- Correlation: Oboke Unit, Nonokawa Formation
- Sedimentary facies: Marine
- Lithofacies: Sandstone
- Lithofacies (Minor): Conglomerate, Interbedded sandstone and shale, Shale
- Thickness: ca. 6,000 m
- Lower limit: Minami-Awa Fault
- Shimanto Belt
- [ Upper ]
- /--/--/--/--/-
- Northern Shimanto Belt
- /--/--/--/--/-
- Southern Shimanto Belt
- ?--?--?--?--?-
- [ Lower ]
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Mizoochi, Mugi city, Kaifu county, Tokushima pref.
- Tsujino et al. (2010) Jour. Geol. Soc. Japan, vol.116, no.12, pp.680-685 DOI
- Yamaguchi et al. (2009) Jour. Geol. Soc. Japan, vol.115, Supplement, pp.21-36 DOI
- Kiminami and Toda (2007) Jour. Geol. Soc. Japan, vol.113, no.4, pp.158-167 DOI