[ Top ] [ Japanese ]
Shimomidani Formation
There are opinions that this formation belongs to Maizuru Belt or Akiyoshi Belt
- Type locality: Shimomidani, Maizuru city, Kyoto prefecture
- Accretionary complex
- Deposition: early - middle Permian
- Intruded by: Oeyama Mass
- Sedimentary facies: Marine
- Lithofacies: Mudstone
- Lithofacies (Minor): Felsic tuff, Conglomerate, Sandstone, Chert
- Lithofacies: Mélange facies, Coherent facies
- Thickness: 1,000 m or thicker
- Thickness (Middle): 600 m
- Thickness (Upper): 1,000 m or thicker
- Upper limit: Unconformity (Hannyaji Formation)
- Distribution: Shimomidani - Okadayuri - Saihoji - Kora - Mount Akaiwayama - Iwao- Kamiurushibara - Jito, Maizuru city, Kyoto pref.; Takatsu - Sogo - Futamata - Naiku, Oe town, Fukuchiyama city, Kyoto pref.; Hidono - Hata - Tokonoo, Tanto, Toyooka city, Hyogo pref.
- Fossils (Radiolarians): Pseudoalbaillella aff. longicornis, Entactinia itsukaichiensis, Ishigaum spp., Cauletella sp., Latentifistula? sp., Latentibifistula? sp., Quadricaulis cf. inflata, Ormistonella cf. adhaerens
- Sugamori (2013) Jour. Geol. Soc. Japan, vol.119 no.5, pp.368-374 DOI
- Igi and Kuroda (1965) Oeyama, Explanatory Text of the Geological Map of Japan, Scale 1:50,000, Geological Survey of Japan, 81p. (in Japanese with English abstract 12p.)