GPS Observations and Modelling of Crustal Deformation in Gulf of Aqaba

Nicolas Castro-Perdomo
The Dead Sea Transform fault (DST) is one of the most prominent tectonic features in the eastern Mediterranean region, located between the Arabian plate and the Sinai sub-plate. Several aspects of this fault system have been thoroughly studied. However, its present-day kinematics along its southern end in Gulf of Aqaba remains poorly understood. This dissertation focusses on crustal motions near Gulf of Aqaba by using geodetic observations and analytical models of crustal deformation. Here we...
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