History of the Kanto earthquakes recorded in marine terraces and tsunami deposits in the southern coast of the Boso Peninsula, central Japan

Author:

Shishikura Masanobu1,Kamataki Takanobu2,Fujiwara Osamu1

Affiliation:

1. Geological Survey of Japan, AIST

2. Regional Disaster Prevention Department, Center for Regional Development, Akita University

Publisher

The Geological Society of Japan

Subject

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

Reference37 articles.

1. Ando, M., 1974, A fault-origin model of the great Kanto earthquake of 1923 as deduced from geodetic data. Bull. Earthq. Res. Inst. Univ. Tokyo, 49, 19–32.

2. 遠藤香織・宮内崇裕(Endo, K. and Miyauchi, T.), 2011, 房総半島南部完新世離水海岸地形の高度と離水年代の再検討-相模トラフ沿いの巨大地震に伴う地震性地殻変動に関連して-.日本活断層学会2011年度秋季 学術大会講演予稿集(Japan Soc. Active Fault Res. Meet. 2011, Abstr.), 52–53.

3. Endo, K., Sekimoto, K. and Takano, T., 1982, Holocene stratigraphy and paleo-environments in the Kanto Plain, in relation to the Jomon Transgression. Proc. Inst. Natural Sciences, Nihon Univ., 21, 37–54.

4. Fujiwara, O., 2014, Traces of paleo-earthquakes and tsunamis along the eastern Nankai Trough and Sagami Trough, Pacific coast of central Japan. Jour. Geol. Soc. Japan, 120, Supplement, 165–184.

5. 藤原 治(Fujiwara, O.), 2015, 津波堆積物の科学(The Science of Tsunami Deposits), 東京大学出版会(Univ. Tokyo Press), 283pp.

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1. A report on the 2019 Tsunami Deposit Workshop;Journal of the Sedimentological Society of Japan;2020-02-25

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