期刊
GEOPHYSICAL RESEARCH LETTERS
卷 44, 期 23, 页码 11833-11839出版社
AMER GEOPHYSICAL UNION
DOI: 10.1002/2017GL075839
关键词
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资金
- Federal Ministry of Education and Research of Germany (BMBF)
- German Research Foundation (DFG)
- JAMSTEC
- Ministry of Education, Culture, Sports, Science, and Technology (MEXT) [JP26000002]
- Grants-in-Aid for Scientific Research [26000002, 15K05278] Funding Source: KAKEN
We conducted multibeam bathymetric surveys crossing the northern Japan Trench offshore Sanriku and examined seafloor displacement by means of the difference in bathymetry before and after the 11 March 2011 Tohoku-oki earthquake. The seafloor displacements were less than several meters in vertical displacement and less than 20 m in trench-normal horizontal displacement; consequently, lower amplitude seafloor displacements were evaluated. Comparatively, the landward lower slope near the trench was uplifted, the middle slope was subsided, and the midslope terrace was depressed after the earthquake. Therefore, localized very large fault slip or very large submarine landslide is unlikely. Instead, smaller uplift of the lower slope near the trench extending broader along the trench seems to be plausible explanation for the devastating tsunami source in the northern Japan Trench area.
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