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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?

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Figure

Fig. 1.(a) Coseismic slip distribution estimated from observed displacements at all GPS stations
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
Fig. 3. The results when we imposed an additional condition that the slip in the Miyagi-oki region is constrained to be zero, and the comparison ofthe residuals between the optimum and the constrained models

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