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K3
- Accretionary complex
- middle - late Eocene
- Intruded by: Quartz porphyry dikes
- Sedimentary facies: Marine
- Lithofacies: Mudstone, Mudstone-dominant interbedded sandstone and mudstone
- Lithofacies (Minor): Sandstone-dominant interbedded sandstone and mudstone, Sandstone, Conglomerate
- Sedimentary structures: Parallel stratification, Scour-fill cross-stratification, Slump structures, Current marks
- Thickness: ca. 400 - 1,300 m
- Kogawa Formation
- [ Upper ]
- /--/--/--/--/-
- K5
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- K4
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- K3
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- K2
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- K1
- /--/--/--/--/-
- [ Lower ]
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Hokusogi - Yomuragawa river - Otogawa river, Tanabe city, Wakayama pref.; Unehata, Shingu city, Wakayama pref.
- Fossils (Shellfishes): Costacallista? sp.
- Fossils (Trace fossils): Paleodictyon isp.
- Suzuki et al (1979) Geology of the Kurisugawa District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 54p. (in Japanese with English abstract 5p.)