F. Gomez et al., Coseismic displacements along the Serghaya fault: an active branch of the Dead Sea Fault System in Syria and Lebanon, J GEOL SOC, 158, 2001, pp. 405-408
Examination of the Serghaya fault, a branch of the Dead Sea Fault System in
western Syria and eastern Lebanon, documents Late Quaternary and Recent le
ft-lateral fault movements including the probable remnant of a historic cos
eismic surface rupture. Carbon-14 dating and the presence of fault-scarp fr
ee faces in soft, late Pleistocene lake deposits suggest coseismic slip dur
ing the past two Or three centuries, possibly corresponding with one of the
well-documented earthquakes of 1705 or 1759, With an estimated Holocene sl
ip rate of 1-2 mm a(-1), the Serghaya Fault accommodates a significant part
of the active deformation along the Arabian-African plate boundary:, These
results suggest that multiple active fault branches are involved in the tr
ansfer of strain through the 'Lebanese' restraining bend.