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- W2023230246 abstract "The recent progress of stratigraphical studies on the Japanese Quaternary has led to the establishment of standard geologic sections (Pliocene-Holocene) of representative basins in Japan and the correlation of each one with the others.In the course of compiling the Quaternary Maps of Japan, the geologic sections were chronostratigraphically subdivided into 5 units, i. e. Pliocene, Lower Pleistocene, Middle Pleistocene, Upper Pleistocene, and, Holocene, based on the definitions approved and/or recommended internationally.Unsolved problems, however, still remain in correlating marine sequences with non-marine sequences, and especially in correlating the Pliocene-Pleistocene boundary in the former with that of the latter.The Kazusa Group, a marine sequence of the Boso Peninsula in Kanto basin, is regarded as an expected hypostratotype section of the Pliocene-Pleistocene boundary. Precise correlations of the Kazusa Group with the Osaka Group of nonmarine-marine origin and the Yamato Group of nonmarine origin, which are well studied bio- and magneto-stratigraphically, are of prime importance. The relation between marine and nonmarine sequences are examinable within the Kanto and Niigata basins, because of the coexistence of both sequences in these basins. Bio- and magneto-stratigraphical and radiometric studies on the Pliocene and Pleistocene in the Kanto and Niigata basins are expected to be completed in the near future." @default.
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- W2023230246 date "1988-01-01" @default.
- W2023230246 modified "2023-10-03" @default.
- W2023230246 title "Subdivision of the Quaternary in Japan" @default.
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- W2023230246 doi "https://doi.org/10.4116/jaqua.26.3_207" @default.
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