[ Top ] [ Japanese ]
Isoura Formation Noda et al., 2010
- Type locality: Isoura village, Niihama city, Ehime prefecture
- Coherent formation
- Izumi sedimentary basin
- Forearc basin associated with strike-slip fault related to Median Tectonic Line
- Late Cretaceous, middle Campanian (Bivalves)
- Sedimentary facies: Main filling of the sedimentary basin
- Lithofacies: Interbedded turbidite and mudstone
- Lithofacies (Upper): Sandstone
- Lithofacies (Upper, Minor): Mudstone, Interbedded sandstone and mudstone
- Lithofacies (Middle): Conglomerate
- Lithofacies (Middle, Minor): Sandstone
- Lithofacies (Lower): Sandstone
- Lithofacies (Bottom): Interbedded sandstone and mudstone
- Sedimentary structures (Middle): Graded bedding
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Isoura village - Hoshigoe village, Niihama city, Ehime pref.; Funaya - Iwaidani, Saijo city, Ehime pref.
- Fossils (Bivalves): Sphenoceramus schmidti, Sphenoceramus sachalinensis, Nucula? sp., Acila (Truncacila) aff. shimojimensis, Nanonavis brevis, Inoceramus (Cordiceramus) yuasai, Inoceramus (Endocostea) bulticus bulticus, Myrtea angularis, Periplomya sp., Yaadia japonica
- Fossils (Ammonoids): Tetragonites cf. popetensis, Gaudryceras sp.
- Noda et al. (2010) Jour. Geol. Soc. Japan, vol.116, no.2, pp.99-113 DOI