Submarine earthquake– and tsunami–induced event deposits
Author:
Affiliation:
1. Geological Survey of Japan, AIST
Publisher
The Editorial Committee of Synthesiology
Subject
General Social Sciences,General Engineering
Link
https://www.jstage.jst.go.jp/article/syntheng/11/1/11_13/_pdf
Reference48 articles.
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2. Y. Okamura: Reconstruction of the 869 Jogan tsunami and lessons of the 2011 Tohoku earthquake: Significance of ancient earthquake studies and problems in announcing study results to society, Synthesiology, 5 (4), 234–242 (2012) (in Japanese) [Synthesiology English edition, 5 (4), 241250 (2012)].
3. J. Uchida, K. Abe, S. Hasegawa and O. Fujiwara: Studies on the source of run-up Tsunami deposits based on foraminiferal tests and their hydrodynamic verification, The Quaternary Research, 46 (6), 533–540 (2007) (in Japanese).
4. K. Oguri, K. Kawamura, A. Sakaguchi, T. Toyofuku, T. Kasaya, M. Murayama, K. Fujikura, R. N. Glud and H. Kitazato: Hadal disturbance in the Japan Trench induced by the 2011 Tohoku-Oki Earthquake, Scientific Reports, 3, 1915, doi: 10.1038/srep01915 (2013).
5. K. Ikehara, T. Irino, K. Usami, R. Jenkins, A. Omura and J. Ashi: Possible submarine tsunami deposits on the outer shelf of Sendai Bay, Japan resulting from the 2011 earthquake and tsunami off the Pacific coast of Tohoku, Marine Geology, 358, 120–127 (2014).
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