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Uridani Formation
- Accretionary complex
- Paleocene (Radiolarians)
- Sedimentary facies: Marine
- Lithofacies: Mudstone
- Lithofacies (Minor): Siliceous mudstone, Green rocks
- Thickness: 30 - 3000 m or thicker
- Upper limit: Bottom of the horizon of interbedded sandstone and mudstone
- Upper limit: Conformity (Haroku Formation)
- Lower limit: Chikatsuyu Thrust fault
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Tondagawa river - Hikigawa river - Otonashigawa river - Mikoshigawa river - Kamoredani valley - Hosshinmon - Michinokawa - Chikatsuyu - Fukusada - Kaoredani valley - Iwasaki - Minanokawa, Tanabe city, Wakayama pref.
- Fossils (Radiolarians): Bathysiphon sp., Cyclogyra? sp., Dentalina sp., Globigerina? sp., Haplophragmoides? sp., Lagena? sp.
- Tokiwa et al. (2016) Jour. Geol. Soc. Japan, vol.122, no.12, pp.625-635, DOI
- Bessho and Nakaya (2011) Jour. Geol. Soc. Japan, vol.117, no.8, pp.423-438 DOI
- Tokuoka et al (1981) Geology of the Ryujin District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 69p. (in Japanese with English abstract 6p.)
- Suzuki et al (1979) Geology of the Kurisugawa District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 54p. (in Japanese with English abstract 5p.)