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Progress in Earth and Planetary Science
Fig. 4 | Progress in Earth and Planetary Science

Fig. 4

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. 4

Comparison of the estimated slip time series with and without “reset after coseismic change.” The figure on the left shows the results of this analysis (a), while that on the right side shows the results without “reset” and switch of smoothing strength (b). Both figures show time series for along dip 13 subfaults crossing the mainshock hypocenter. Red lines represent updip 5 subfaults, and blue lines represent downdip 8 subfaults, respectively. The figures cover the entire analysis period, setting the mainshock origin as zero. Black vertical lines represent the origin times of the mainshock and three major aftershocks

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