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Three hundred and ten faults, most with slips of < 2 m, were observed along 3 km of seacliffs near an active dextral-reverse fault. The density of post-early Pliocene faults increases with proximity to this major fault. Most faults are oblique-normal. Younger dextral-reverse faults have larger displacements and are concentrated in a ∼300 m wide zone bordering the active fault. Distribution of...
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