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The existence of a mechanical barrier (in the case of their study, a segment boundary) prevents the simultaneous rupture of the two segments.
In the mutant with two symmetrical hydrogen bonds (FM197H) a single cooperative rupture of the two bonds was observed corresponding to an about twice stronger bond, rather than a sequential rupture of two individual bonds.
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The kinematic source rupture processes of the two earthquakes were estimated with the multiple time-window linear waveform inversion method (Hartzell and Heaton 1983; Olson and Apsel 1982).
This paper focuses on the source rupture processes of the two significant events during the 2016 Kumamoto earthquake sequence based on kinematic waveform inversion analyses using strong motion data.
The rupture areas of the two earthquakes are nearly identical, and the 5-m seismic slip of the 2003 event is consistent with the slip deficit accumulated over the 51 years from 1952 to 2003, assuming a subduction rate of ~10 cm/year.
We applied the same procedure as that detailed in the previous section to the rupture areas of the two other M9-class earthquakes that occurred in the 20th century; i.e., the 1952 Mw9.0 Kamchatka earthquake and the 1964 M9.2 Alaska earthquake (in addition to the 1960 Mw9.5 Chile earthquake).
In the eight pregnancies in which amnioreduction was not performed, one pregnancy was complicated by premature rupture of the membrane, two pregnancies presented with mild TTTS (stage I), and one pregnancy opted for delivery.
Among the factors involved in the modulation and/or permanent aperture of the MPT pore and rupture of the OMM, three groups are of key importance.
Therefore, to be consistent with the previous study, we adopted the F-net seismic moment and a logarithmic average of the rupture areas of the three models for the scaling relationship of seismic moment versus rupture area.
Figure 5a c shows the distribution of the calculated magnitude around the rupture areas of the three M9-class events.
The large red triangle represents the logarithmic average of the rupture areas of the three models for the 2016 Kumamoto earthquake (M w 7.0) shown in Table 1.
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