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Earth, Planets and Space
Fig. 10 | Earth, Planets and Space

Fig. 10

From: Simulation of great earthquakes along the Nankai Trough: reproduction of event history, slip areas of the Showa Tonankai and Nankai earthquakes, heterogeneous slip-deficit rates, and long-term slow slip events

Fig. 10

Distributions of (left) slip velocity and (right) slip-deficit rate on the plate interface southeast of Cape Shiono at six points in time before and during the quasi-Hoei-type earthquake (events 95–97) which followed the Showa-type earthquake of events 92 and 93. Slip velocity is normalized by the plate convergence rate. The quasi-Hoei-type event (see Fig. 5) consisted of a Tonankai event (95), Nankai event (96) and Hyuganada event (97). Plots depict a, b ~ 20 years before and c, d ~ 1 year before event 95; e, f the start of event 95 (epicenter shown by star) g, h immediately and i, j ~ 270 days after event 95, and k, l the start of event 96 (epicenter shown by star)

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