[ Top ] [ Japanese ]
Nina Formation
- Coherent formation
- Foreland basins by collision between northeast Japan island arc and Kuril island arc
- late Miocene - Pliocene (Diatoms)
- Sedimentary facies: Fan delta front
- Sedimentary facies (Lower): Shoot and Levee
- Depth of water: Continental shelf
- Lithofacies: Turbidite
- Lithofacies: Siltstone, Mudstone, Interbedded turbidite sandstone and siliceous siltstone
- Lithofacies (Minor): Sandstone, Conglomerate
- Sedimentary structures: High angle foreset cross stratification
- Paleocurrent: Southwest
- Hidaka basin, northeast
- [ Upper ]
- ?--?--?--?--?-
- Niniu Group
- ?--?--?--?--?-
- [ Lower ]
- Hidaka basin, southwest
- [ Upper ]
- ?--?--?--?--?-
- Fureoi Formation
- ?--?--?--?--?-
- [ Lower ]
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Asahioka, Mukawa city, Yufutsu county, Hokkaido; Midorimachi, Hidaka city, Hidaka county, Hokkaido
- Kase et al., (2018) Jour. Geol. Soc. Japan, vol.124, no.8, pp.627-642 DOI