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- W2320442967 abstract "Two fine vitric tephra layers of middle Holocene age are recognized in peaty surface soil on Mt. Tide. The lower one is identified as the Kikai-Akahoya ash (K-Ah, about 6, 300y.B.P.) on the basis of type, refractive index, and major element chemical composition of volcanic glass shards and 14C age. The upper one is called the Azuma ash (Az) and has some similarities to Towada-Chuseri ash (To-Cu, about 5, 400y.B.P.), although further inspection is necessary.Az can be seen at many localities on the Tide and Asahi Mountains. These tephras, especially Az, would be useful in chronological study of slope formation in these areas." @default.
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- W2320442967 date "1988-01-01" @default.
- W2320442967 modified "2023-10-06" @default.
- W2320442967 title "The middle Holocene tephras on the Iide and Asahi mountains and their implication to slope chronology." @default.
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- W2320442967 doi "https://doi.org/10.5026/jgeography.97.6_611" @default.
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