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. 2018 Sep 11;8:13620. doi: 10.1038/s41598-018-31956-8

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© The Author(s) 2018

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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Seismic profiles of forearc slopes seaward of the Sakishima Islands. (a) Seismic profile of ECr4, which shows the topographic high bounding the seaward margin of the accretionary prism. (b) Seismic profile of ECr5, in which the seaward topographic high is absent. Approximate locations of the fault models^23,25 for the 1771 tsunami source are shown by dashed lines above the forearc basin. Locations of the profiles are shown in Fig. 1. The image was produced using SPW 2.2 [http://www.parallelgeo.com/] and Adobe Illustrator CS6.