Stratigraphic correlation between the lower Pleistocene Chikura Group in the southern part of the Boso Peninsula and the Kazusa Group in the eastern part of the peninsula, based on magneto- and tephro-stratigraphy-Reference-Cited by-同舟云学术

Stratigraphic correlation between the lower Pleistocene Chikura Group in the southern part of the Boso Peninsula and the Kazusa Group in the eastern part of the peninsula, based on magneto- and tephro-stratigraphy

Published:2023-10-31 Issue:1 Volume:129 Page:469-487
ISSN:0016-7630
Container-title:The Journal of the Geological Society of Japan
language:en
Short-container-title:Jour. Geol. Soc. Japan

Author:

Konishi Takumi¹,Utsunomiya Masayuki²,Okada Makoto³,Tamura Itoko⁴

Affiliation:

1. Yachiyo Engineering Co., Ltd.

2. Geological Survey of Japan, AIST

3. Graduate School of Science and Engineering, Ibaraki University

4. Chuo University

Publisher

The Geological Society of Japan

Subject

General Earth and Planetary Sciences,General Engineering,General Environmental Science

Link

https://www.jstage.jst.go.jp/article/geosoc/129/1/129_2023.0014/_pdf

Reference48 articles.

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3. Haneda, Y. and Okada M., 2022, A record of the lower Mammoth geomagnetic polarity reversal from a marine succession in the Boso Peninsula, central Japan. Geophys. J. Int., 228, 461–476.

4. 林広樹・堀内誠示・高橋雅紀・笠原敬司, 2004, 関東平野地下に分布する新第三系の層序と対比．石技誌, 69, 404–416. ［Hayashi, H., Horiuchi, S., Takahashi, M. and Kasahara, K., 2004, Stratigraphic correlation of subsurface Neogene deposits in the Kanto Plain, Central Japan. J. Japan. Assoc. Pet. Technol., 69, 404–416.］

5. Ito, M. and Katsura, Y., 1992, Inferred glacio-eustatic control for high-frequency depositional sequences of the Plio-Pleistocene Kazusa Group, a forearc basin fill in Boso Peninsula, Japan. Sediment. Geol., 80, 67–75.