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Fig. 2. | Earth, Planets and Space

Fig. 2.

From: Coseismic slip distribution of the 2011 off the Pacific coast of Tohoku Earthquake (M 9.0) estimated based on GPS data—Was the asperity in Miyagi-oki ruptured?

Fig. 2.

Comparison between observed displacements (black arrows in (a) and bars in (b) ) and calculated ones (white arrows in (a) and bars in (b) ) from the estimated coseismic slip distribution. (a) Horizontal component and (b) vertical component are shown with their residuals ((c) and (d)). The residuals are calculated by subtracting the calculated displacement from the observed displacement for each site.

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