[ Top ] [ Japanese ]
K1
- Accretionary complex
- middle - late Eocene
- Intruded by: Acidic pyroclastic dikes
- Sedimentary facies: Marine
- Lithofacies: Mudstone
- Lithofacies (Minor): Mudstone-dominant interbedded sandstone and mudstone, Conglomerate, Gravel-bearing mudstone
- Sedimentary structures: Cross stratification
- Thickness: 150 - 800 m
- Sedimentary structures: Flute marks
- Paleocurrent: to South
- Kogawa Formation
- [ Upper ]
- /--/--/--/--/-
- K5
- --------------
- K4
- --------------
- K3
- --------------
- K2
- --------------
- K1
- /--/--/--/--/-
- [ Lower ]
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Komori - Oze - Takayamadani valley - Kurozodani valley - Sasanose, Tanabe city, Wakayama pref.; Unehata, Shingu city, Wakayama pref.
- Fossils (Shellfishes): Acila (Truncacila) sp.
- Fossils: Trace fossils, Pipe rocks
- 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.)
- 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.)