Reported fault slip rates, a key quantity for earthquake hazard and risk analyses, have been
inconsistent for the northern Dead Sea fault (DSF). Studies of offset geological and …

The present‐day motions in and around the Arabian plate involve a broad spectrum of
tectonic processes including plate subduction, continental collision, seafloor spreading …

Large earthquakes (magnitude≥ 7.0) are rare, especially along slow-slip** plate
boundaries. Lack of large earthquakes in the instrumental record enlarges uncertainty of the …

Abstract The East Anatolian Fault (EAF), Cyprus Arc and Dead Sea Fault (DSF) intersect at
the Hatay Triple Junction (HTJ) in southern Turkey, which is a tectonically controversial zone …

Abstract Interferometric Synthetic Aperture Radar (InSAR) data are increasingly being used
to map interseismic deformation with ascending and descending‐orbit observations …

Temporal distribution of earthquakes is key to seismic hazard assessment. However, for
most fault systems shortness of large earthquake catalogues makes this assessment difficult …

We present a methodology for map** faults that constitute a potential hazard to structures,
with an emphasis on ground shake hazards and on surface rupture nearby critical facilities …

Crustal deformation and seismic activity in the Levant is mainly related to the interplate Dead
Sea Fault (DSF) and the intraplate Carmel–Gilboa Fault System (CGFS). In this study, we …

SUMMARY A comprehensive GPS velocity field along the Dead Sea Fault System (DSFS)
provides new constraints on along-strike variations of near-transform crustal deformation …

The geodynamic evolution of the Sinai Triple Junction, a highly deformed and seismically
active area, is controlled by the Red Sea rift, Gulf of Suez and Aqaba-Dead Sea …