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N4
- Type locality: Sakatai - Kazai - Kshokuchi, Tanabe city, Wakayama prefecture
- Accretionary complex
- Paleogene, or Late Cretaceous, Campanian
- Sedimentary facies: Marine
- Sedimentary facies: Continental shelf, Upper continental slope
- Lithofacies: Sandstone-dominant interbedded sandstone and mudstone
- Lithofacies (Middle, Minor): Mudstone-dominant interbedded sandstone and mudstone
- Lithofacies (Minor): Conglomerate, Gravel-bearing mudstone, Greenstones
- Sedimentary structures: Graded bedding, Parallel structure, Wave ripples, Flute marks, Groove marks
- Paleocurrent (Lateral current flow): to North - Northwest
- Thickness: 300 - 640 m or thicker
- Upper limit: Bottom of a thick sandstone bed
- Nyunokawa Formation
- [ Upper ]
- /--/--/--/--/-
- N5
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- N4
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- N3
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- N2
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- N1
- /--/--/--/--/-
- [ Lower ]
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Sakatai - Kazai - Kshokuchi - Wadamori - Mitsumatadani valley - Ogyoji - Mount Andosan, Tanabe city, Wakayama pref.; Kamiyukawa river - Teragaito - Obiso - Tonoi, Totsukawa city, Yoshino county, Nara pref.
- Tokuoka et al (1981) Geology of the Ryujin District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 69p. (in Japanese with English abstract 6p.)