[ Top ] [ Japanese ]
Koetoi Formation (Watanabe, 1914) Fukuzawa, 1985
- Coherent formation
- Foreland basins by collision between northeast Japan island arc and Kuril island arc
- late Miocene - Pliocene
- Sedimentary facies: Marine
- Lithofacies: Siliceous mudstone, Diatomaceous mudstone
- Lithofacies (Upper): Sandy
- Lithofacies (Minor): Tuff
- Sedimentary structures: Unclear bedding planes
- Upper limit: Bottom of muddy sandstone bed
- Upper limit: Conformity (Yuchi Formation)
- Lower limit: Bottom of the bed with unclear bedding planes
- Lower limit (previous definition): boundary of Opal-A/Opal-CT
- Lower limit: Transitional (Wakkanai Formation)
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Soya region, Hokkaido
- Distribution: Horonobe city, Teshio county, Hokkaido
- Fossils: Shellfishes, Diatom (Neodenticula kamtschatica)
- Kase et al., (2018) Jour. Geol. Soc. Japan, vol.124, no.8, pp.627-642 DOI
- Ishii et al. (2008) Jour. Geol. Soc. Japan, vol.114, no.6, pp.286-299 DOI
- Ishii et al. (2007) Jour. Geol. Soc. Japan, vol.113, no.2, pp.41-52 DOI
- Niizato et al. (2007) Jour. Geol. Soc. Japan, vol.113, Supplement, pp.119-135 DOI