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b Distribution of rupture velocity.
The map shows the distribution of rupture segments of Nankai Trough earthquakes.
Force spectroscopy measurements of the rupture of the molecular bond between biotin and streptavidin often results in a wide distribution of rupture forces.
The distribution of sand bodies and the thickness of sandstone layers have a distinct impact on the distribution of rupture values within the Longdong area.
Thus, the spatial distribution of rupture speed determined in this study (Fig. 3) may be interpreted in terms of differences in dynamic friction on the fault.
The spatio-temporal distribution of rupture fronts suggests that the earthquake ruptured northeastwards and southwestwards over a total length of more than 340 km during at least 143 s.
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It is shown that the measured distributions of rupture forces still contain high forces that cannot be described by the forced dissociation from a deep potential well.
Upper map shows distribution of six rupture segments along Nankai Trough.
Then, multi-scale heterogeneity is added to the spatial distribution of the rupture velocity of Model H1 to yield Model H2.
Gray areas indicate the distribution of the rupture areas of large shallow earthquakes (depth ≤60 km) with a magnitude of 7 or greater (1926 1987) (Umino et al., 1990; Ammon et al., 2011).
Among the three parameters to which heterogeneity was added, the spatial distribution of the rupture velocity showed the largest influence on the ground motion, which is consistent with Watanabe et al. (2008).
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