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For the discussion, we define the term "moment deficit rate" or MDR, which means the moment of the slip deficit rate on the plate interface.
The estimated moment deficit rate (MDR) is larger than that expected from the asperity distribution.
We therefore made the assumption that the deficit rate is zero tentatively.
We call Δw s (x, t) the slip deficit rate hereafter.
Black arrows indicate the estimated slip deficit rate distribution by geodetic data inversion.
In these parts, the solution of the slip deficit rate is strongly influenced by the boundary condition.
Using the real geodetic data, the estimates for the slip deficit rate distribution are shown in Fig. 12.
The estimated slip deficit rate distribution and the observed and reproduced velocity are also shown in the figure.
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The initial stress distribution is obtained from the slip-deficit rate.
Hashimoto et al. (2009) deduced the slip-deficit rate distribution along the Nankai Trough using GPS Earth Observation Network GEONETT) data for 4 years, which Hok et al. (2011) used to calculate the accumulated slip-deficit rate for 100 years.
Fig. 11 Comparison of the coseismic slip distribution of the Genroku event with the interseismic slip-deficit rate distribution.
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