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Fig. 7 | Earth, Planets and Space

Fig. 7

From: Slip parameters on major thrusts at a convergent plate boundary: regional heterogeneity of potential slip distance at the shallow portion of the subducting plate

Fig. 7

Results of numerical simulations of heating during fault slip used to determine the amounts of slip necessary to achieve the target temperatures. a 700 ± 100 °C in the ultracataclasite layer in the Emi major thrust. b 1300 ± 100 °C in the pseudotachylyte layer in the Kure OST for different slip rates and depths of burial. Slip distances during three historical earthquakes are referred from Ando (1975) and Furumura et al. (2011)

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