Tsunami deposits from the 1640 Hokkaido Komagatake eruption, north Japan: constraints on inundation heights and numerical simulation of volcanic debris avalanche-derived tsunami
Author:
Affiliation:
1. Atmosphere and Ocean Research Institute, Tokyo University
2. Hokkaido Soil Research Co-operation
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/125/12/125_2019.0032/_pdf
Reference39 articles.
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2. 阿部勝征, 1999, 遡上高を用いた津波マグニチュードMtの決定-歴史津波への応用-.地震第2輯, 52, 369–377. [Abe, K., 1999, Quantification of historical tsunamis by the Mt Scale. J. Seismol. Soc. Japan, 2nd Ser. 52, 369–377.]
3. 相田 勇, 1977, 三陸沖の古い津波シミュレーション.東京大學地震研究所彙報, 52, 71–101. [Aida, I., 1977, Simulations of large tsunamis occurring in the past off the coast of the Sanriku district. Bull. Earthquake Res. Inst., Univ. Tokyo, 52, 71–101.]
4. Baba, T., Takahashi, N., Kaneda, Y., Ando, K., Matsuoka, D. and Kato, T., 2015, Parallel implementation of dispersive tsunami wave modeling with a nesting algorithm for the 2011 Tohoku Tsunami. Pure Appl. Geophys., 172, 3455–3472.
5. Folk, R. L. and Ward, W. C., 1957, Brozos River Bar: A study in the significance of grain size parameters. J. Sediment. Petrol., 27, 3–26.
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