WebApr 1, 2024 · The main rupture corresponding to the strike-slip mechanism is located within the gulf of Aqaba, which forms the marine extension of the Levantine fault, also known as the Dead Sea fault. WebJul 3, 2014 · The Dead Sea transform is an active plate boundary connecting the Red Sea seafloor spreading system to the Arabian-Eurasian continental collision zone. Its …
Active tectonics of the northern Dead Sea Fault System …
WebSep 1, 2000 · The fault segment that extends along the Araba valley south of the Dead Sea seems to depart from the rest of the fault zone.This 160-km-long fault zone has produced only a few large-magnitude earthquakes (), in spite of its significant 4 ± 2 mm yr −1 slip rate (Klinger 1999; Klinger et al. 2000).This may suggest a particular seismic behaviour … WebJan 1, 2014 · The Dead Sea Fault (DSF) is an active transform fault linking opening in the Red Sea with collision in the Taurus/Zagros Mountains. Motion is left-lateral and … team leader work from home jobs
Travels in Geology: The Dead Sea Rift: Salty soaks and …
WebThe Dead Sea Transform (DST) fault system, also sometimes referred to as the Dead Sea Rift, is a series of faults that run from the Maras Triple Junction (a junction with the East Anatolian Fault in southeastern Turkey) to the northern end of the Red Sea Rift (just offshore of the southern tip of the Sinai Peninsula). ... The Dead Sea Transform (DST) fault system, also sometimes referred to as the Dead Sea Rift, is a series of faults that run from the Maras Triple Junction (a junction with the East Anatolian Fault in southeastern Turkey) to the northern end of the Red Sea Rift (just offshore of the southern tip of the Sinai Peninsula). … See more The DST fault system is generally considered to be a transform fault that has accommodated a 105 km northwards displacement of the Arabian Plate. This interpretation is based on observation of offset markers, … See more The Dead Sea Transform began to form during the Late Eocene with epeirogenic movement in the region, with the start of the faulting phase beginning in the Oligocene and continuing into the Miocene. During the Early to Middle Miocene (23–11.6 Ma), … See more • Castro-Perdomo, Nicolás; Viltres, Renier; Masson, Frédéric; Klinger, Y.; Liu, S.; Dhahry, M.; Ulrich, P.; Bernard, J.; Matrau, R.; Alothman, A.; Zahran, H.; Reilinger, R.; Mai, P. M.; Jónsson, S. (2024). "Interseismic deformation in the gulf of aqaba from GPS … See more Southern section The southern section of the DST is about 400 km long, extending from the spreading center in the Red … See more • 1138 Aleppo earthquake • Beqaa Valley • Great Rift Valley (geographical concept) • Jordan Rift Valley See more sowers landscape