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Fig. 1 | Earth, Planets and Space

Fig. 1

From: Submarine terraces reveal Late Quaternary tectonic deformation in the intermediate zone between the island shelf and rift zone of the middle part of the Nanseishoto Islands, southwest Japan

Fig. 1

Index map of the study area (A, B) and using data from this study (c). Shaded relief maps overlain by contour maps (A and B) use a 500 m mesh DEM (J-EGG500) from the Japanese Coast Guard (JCG), a 1-degree mesh DEM (ETOPO 1) provided by the National Center for Environmental Information (USA), and inland SRTM-3 data provided by the US Geological Survey (USGS). Red lines in B indicate active fault lines identified by the Research Group for Active Faults in Japan (1991), Arai et al. (2015), Goto et al. (2018), and Honza et al. (1977). C-1: 0.65-s-mesh DEM of Sato et al. (2013) and onshore SRTM-3 data provided by the USGS, C-2: 1.44-s-mesh DEM of Yasuhara (2013) and C-1, C-3: 2.03-s-mesh DEM data from the Darwin website of the Japan Agency for Marine-Earth Science and Technology (JAMSTEC) and C-2, C-4: 2.08-s-mesh DEM produced from the contour lines on the chart of the Japan Hydrographic Association and C-3, C-5: 9.69-s-mesh DEM of the J-EGG500 from JCG and C-4

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