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Nagao Formation Mori, 1947
- Type locality: Oppa river, Ishinomaki city, Miyagi prefecture
- Coherent formation
- Middle Jurassic, Bajocian - Late Jurassic, Tithonian
- Intruded by: Tatebitoge Mass
- Sedimentary facies:
- Lithofacies (Main part): Shale
- Lithofacies (Lower): Sandstone
- Sedimentary structures (Main part): Convolute lamination
- Sedimentary structures (Lower): Slump structures
- Thickness: ca. 500 - 800 m
- Thickness (Main part): 500 m or thicker
- Thickness (Lower): ca. 20 - 150 m
- Upper limit: Unconformity (Yoshihama Formation)
- Lower limit: Conformity (Nakahara Formation)
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Oppa river, Ishinomaki city, Miyagi pref.; Okinagura creek - Nagaohigashi creek - Tsukihama creek - Honji - Izumisawa - Nakahara - Jusanhama, Kitakami town, Ishinomaki city, Miyagi pref.; Mitobe river, Shizukawa, Minamisanriku city, Motoyoshi county, Miyagi pref.
- Fossils: Belemnoids, Bivalves
- Fossils (Ammonoids): Garantiana sp., Holcophylloceras spp., Kepplerites sp., Kranaosphinctes sp., Leptosphinctes sp., Lytoceras cf. neumayri, Normanites sp., Otoites sp., Stephanoceras sp., Taramelliceras sp., Berriasellidae or Olcostephanidae
- Fossils (Radiolarians): Archaeodictyomitra sp., Cinguloturris cf. carpatica, Dictyomiitrella? cf. kamoensis, Dicryomiterella cf. kamoensis, Eucyrtidiellum sp., Hsuum sp., Parvicingula sp., Protunuma sp., Stichocapsa convexa, Tricolocapsa? fusiformis, Tricolocapsa plicarum
- Takizawa et al. (1990) Geology of the Toyoma District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 126p. (in Japanese with English abstract 8p.)