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Associated with this are many fault segments.
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.
Rift-parallel fault segments were reactivated by reverse slip whereas rift-oblique fault segments were reactivated as oblique-slip faults or lateral/oblique ramps.
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.
Propagation of fault segments is accommodated by dilational fractures nucleating at their respective tips.
From there it spread to the other fault segments within about 3 s.
Three fault segments are recognized by this study, compared with the two segments recognized previously.
The estimated total vertical displacement on certain northern and southern fault segments exceeds 450 m.
The result shows that fault segments have been reactivated by dip-linkage.
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