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Fig. 6 | Progress in Earth and Planetary Science

Fig. 6

From: Deep-sea bottom-water environment change caused by sediment resuspension on the continental slope off Sanriku, Japan, before and after the 2011 Tohoku Earthquake

Fig. 6

Time series of DO in the bottom water at the deep-sea station (~ 1000 m depth) off Otsuchi Bay (Fig. 1a) before and after the events of the large earthquakes (purple double lines): February 17, 2015 (Ev1, Fig. 1a), September 17, 2017 (Ev2, Fig. 1a), and July 7, 2018, off then Boso Peninsula (Ev3). Dashed and bold lines refer to the 9-day mean values before and after the large earthquakes, respectively

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