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It suggests that multiple fault segments may have been ruptured around this area.
The 2016 moment magnitude (Mw) 7.8 Kaikoura earthquake demonstrated that multiple fault segments can undergo rupture during a single seismic event.
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Yoshida et al. (2016) conducted a two-step approach for multiple time-window kinematic waveform inversions of strong-motion data to estimate detailed slip distributions on these four fault segments.
Associated with this are many fault segments.
The NNE faults consist of right-stepping sinistral strike-slip fault segments (e.g. Sin El Kiddab fault).
Steeply dipping fault segments contain rhombohedral calcite veins that cross the fault zone obliquely, parallel to shear segments in mudrock.
Three fault segments are recognized by this study, compared with the two segments recognized previously.
Three fault segments with the reddest colors - hence the greatest likelihoods of rupture - stand out.
Fortunately, both of these fault segments cross areas with relatively sparse population.
Each fault zone has typical self-similar strike-slip architecture comprising multi-scale fault segments.
New fault segments form as well, resulting in complex 3-D fault zone architecture.
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