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

Fig. 2

From: Continuous estimation of coseismic and early postseismic slip phenomena via the GNSS carrier phase to fault slip approach: a case study of the 2011 Tohoku-Oki sequence

Fig. 2

Examples of the estimated slip time series. Now, we show time series for three subfaults near the hypocenter of the Iwate-Oki EQ (a), mainshock (b), and Ibaraki-Oki EQ (c), as indicated by black squares in Fig. 1. The figures describe the slip time series calculated from the estimated values of two slip basis. All figures cover the whole analysis period and use GPS Time. Vertical lines indicate the origin time of the mainshock and three significant aftershocks. Please note that the scale of the vertical axis differs for each figure

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