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c Average slip rate across each patch.
c Average slip rate for each patch.
Thin black lines show the average slip rate attributable to short-term SSEs in each region.
Gray lines show the average slip rate attributable to short-term SSEs observed geodetically in the northern area.
We also assess the relation among the average slip rate, the convergence rate at the trench, and the slip deficit rate in the transition zone.
They showed that the average slip rate became higher in the accelerated period of the Tokai long-term SSE (Ozawa et al., 2002).
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The time of fault onset ranges between 5.3 and 2.2 Myr; overall the average slip rates of the various thrusts are in the range of 0.26 1.35 mm/yr.
The estimated average slip rates are 3.0±0.4 cm/yr, 2.6±0.4 cm/yr, and 2.4±0.4 cm/yr, in the northern, central, and southern Kii Peninsula, respectively.
The shortening rate from geodetic surveys is very close to the averaged slip rate, indicating that geodetic interseismic deformation is essentially elastic and released by slip on the thrust fault (Ader et al. 2012).
The average fault slip rate since eruption is simply determined by dividing the average offset by the eruption age (Bradley et al. 2017; Sieh and Natawidjaja 2000).
This supports the smaller average vertical slip rate of the segment.
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