Earthquakes occur during movement along plate boundaries and active faults. Evaluation of seismic hazards on active faults relies on the understanding of seismic histories and rates of the current deformation. However, in some fault zones large earthquakes have long recurrence periods (> 100-10,000 years; e.g., Tian Shan, China; Charlevoix, Quebec), and thus past seismic statistics […]
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