Sedimentary processes and depositional environments of a continuous marine succession across the Lower-Middle Pleistocene boundary: Kokumoto Formation, Kazusa Group, central Japan
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| 形式 | 参考書籍・資料 |
|---|---|
| 著者 | 西田尚央, 風岡修, 泉賢太郎, 菅沼悠介, 岡田誠, 吉田剛, 荻津達, 中里裕臣, 亀山瞬, 香川淳, 森崎正昭, 楡井久 |
| オンライン版公開日 | 2015年7月14日 |
| 掲載誌 | Quaternary International |
購入先
The Chiba composite section of the Kokumoto Formation in central Japan is a remarkable, thick marine succession and is a candidate for formal recognition as the Global Boundary Stratotype Section and Point (GSSP) for the base of the Middle Pleistocene stage. Although there have been numerous studies of the Kokumoto Formation, the sedimentology of the formation, particularly in the Chiba composite section, has been unclear.Sedimentary processes and depositional environments of a continuous marine succession across the Lower–Middle Pleistocene boundary: Kokumoto Formation, Kazusa Group, central Japan – ScienceDirect
