Paleoseismic History of the Dead Sea Fault Zone
Résumé
The aim of this entry is to describe the DSF as a transform plate boundary pointing out the rate of active
deformation, fault segmentation, and geometrical complexities as a control of earthquake ruptures. The
distribution of large historical earthquakes from a revisited seismicity catalogue using detailed
macroseismic maps allows the correlation between the location of past earthquakes and fault segments.
The recent results of paleoearthquake investigations (paleoseismic and archeoseismic) with a recurrence
interval of large events and long-term slip rate are presented and discussed along with the identification of
seismic gaps along the fault. Finally, the implications for the seismic hazard assessment are also discussed.
Origine : Fichiers produits par l'(les) auteur(s)
Loading...