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Progress in Earth and Planetary Science
Fig. 2 | Progress in Earth and Planetary Science

Fig. 2

From: Heterogeneous rheology of Japan subduction zone revealed by postseismic deformation of the 2011 Tohoku-oki earthquake

Fig. 2

Decade-long geodetic observations after the 2011 Tohoku-oki earthquake around NE Japan. a The location of onshore and offshore geodetic stations. b Displacement rate during April 2011–April 2014, c April 2014–April 2017, and d April 2017–April 2020. Note that only high-quality data of 110 GEONET stations is plotted and horizontal motion during 2011–2014 is scale down to one half in (b). The displacement rate at JCG and TU GNSS-A sites is opted from Honsho et al. (2019) and Watanabe et al. (2021). The displacements of inland GNSS stations are referenced to Fukue station (ID: 950,462; 128.843°E, 32.669°N)

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