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This result corresponds to our assumption of the existence of an interseismi-cally stable (not strongly locked) region near the trench, part of which is the TP region.
This finding may indicate that the fault in the whole shallow part had not been strongly locked in an interseismic phase.
If the extremely large slip of the Tohoku earthquake in the shallow part is associated with dynamic fault weakening, as demonstrated in this study, a strongly locked area during interseismic periods is not necessarily needed for the occurrence of megaquakes.
In the Nankai subduction zone, seismogenic faults at depths of 5 25 km are strongly locked, although locking at the transition zone at depths of 25 35 km, where short-term SSEs and nonvolcanic DLF tremors are located, is weaker than at shallow depths (Tabei et al., 2007).
The consistency in the population allows us to focus subsequent analyses on the phase locking of strongly locked neurons.
Rare examples of neurons strongly locked to retraction could be artifacts from locking of whisking and vocalization.
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A fleshly actor could not convey more strongly the locked joints and the limbs stiffened with pain.
However, this difference between strongly and weakly locked neurons is less pronounced for CCs (63% vs. 32%) and further decreases for UEs (65% vs. 46%).
The conservation of the locking of UE spikes in strongly and weakly locked neurons compared with the declines for ISO and CC hints at different dynamical origins of the coincident spikes in CC and UE. Figure 4 C confirms that individual neurons are consistent with the findings for population ratios (Fig. 4 B ).
An interseismic long-term fault coupling investigation (Fig. 8a) and geodetic studies revealed that the Wellington region was highly locked and strongly aseismic in the decades before the 2016 Kaikoura earthquake (Wallace 2004; Wallace and Beavan 2010).
We find that in the independent coding model the optimal peer prediction timescale depends strongly on phase locking.
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