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The average slip (relative motion) between the two plates during the earthquake was approximately 5 m (16 ft), and the maximum slip was approximately 20 m (66 ft).
The estimated maximum slip was approximately 40%% less than the true value.
Using the InSAR data only, Tobita et al. (2011) showed that their resultant maximum slip was also in agreement with this value.
SC02 had the smallest moment magnitude (Mw 8.5) among the four models, whereas the maximum slip was much larger than for SC01.
A large-slip (> 4 m) area with the maximum slip was found north of Kathmandu (from 60 to 100 km east-southeast of the hypocenter).
The estimated maximum slip was one-and-a-half times greater than the value of true slip in the case of the shallower peak, while it was five times larger than the value of true slip for the deeper peak.
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The maximum slip is about 28 m if the rigidity is assumed to be 30 GPa.
The maximum slip is found to occur deeper than the epicenter (143.3, 38.3) (JMA, 2011).
The maximum slip is larger in the regional analysis because of a spatially finer resolution.
The maximum slip is about 24 m for case 300_3 and 20 m for case 400_5.
The seismic moment and maximum slip were estimated as 5.5 × 1019 Nm (M w 7.1) and 3.8 m, respectively.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com