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Fig. 10 | Earth, Planets and Space

Fig. 10

From: Source process with heterogeneous rupture velocity for the 2011 Tohoku-Oki earthquake based on 1-Hz GPS data

Fig. 10

Comparison between observed and synthetic static coseismic displacements, shown as red and black arrows, respectively, for hr-GPS stations, with average displacement of 270–300 s, and OB-GPS stations. The weight of OB-GPS data relative to hr-GPS data is 100. The left-hand figure shows a comparison of horizontal displacements with legends of 10 m for OB-GPS stations and 2.5 m for hr-GPS stations; that on the right shows a comparison of vertical displacements with legends of 2 m for OB-GPS stations and 0.5 m for hr-GPS stations

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