[ Top ] [ Japanese ]
Aburatsubo Pyroclastic Rock Member (Akamine et al., 1956)
- Coherent formation
- Pliocene (ca. 5 - 3 Ma)
- Sedimentary facies: Marine
- Lithofacies: Pyroclastic rock dominant interbedded sandy siltstone/silty sandstone and scoria/scoriaceous tuff
- Thickness: 100 - 150 m
- Upper limit: Conformity (Hatsuse Formation)
- Upper limit: Bottom of Sj22 Tephra Bed
- Misaki Formation
- [ Upper ]
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- Aburatsubo Pyroclastic Rock Member
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- Lower part
- ?--?--?--?--?-
- [ Lower ]
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Sajima, Yokosuka city, Kanagawa pref.
- Tephra: So
- Mori and Ogawa (2019) Jour. Geol. Soc. Japan, vol.125, no.10, pp.737-757 DOI
- Eto et al. (1998) Geology of the Yokosuka District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 128p. (in Japanese with English abstract 3p.)
- Kodama et al. (1980) Geology of the Misaki District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 38p. (in Japanese with English abstract 3p.)