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Segev, A., Rybakov, M., Lyakhovsky, V., Hofstetter, A., Tibor, G., Goldshmidt, V., & Ben Avraham, Z. (2006). The Structure, Isostasy and Gravity Field of the Levant Continental Margin and the Southeast Mediterranean Area. Tectonophysics, 425, 137-157.
https://doi.org/10.1016/j.tecto.2006.07.010

has been cited by the following article:

• TITLE: Evaluation of the Crustal Features of the Gulf of Aqaba Deduced from Geophysical Data

  AUTHORS: A. Z. Hamouda, S. El-Gharabawy

  KEYWORDS: Gulf of Aqaba, Bouguer Map, Bathymetry, Crustal Thickness, Moho Discontinuity, Tectonics Activity, Red Sea

  JOURNAL NAME: Journal of Geoscience and Environment Protection, Vol.7 No.4, April 17, 2019

  ABSTRACT: The Gulf of Aqaba is considered as an interesting rift system. Therefore, it is important to understand the crustal features and thickness variation along the Gulf; to be able to evaluate the effect of tectonic activities in shaping the Gulf. The obtained data were used to estimate the reliable empirical relations between the Bouguer anomalies (ΔgB) and crustal thickness (Hc) in the Gulf of Aqaba. This equation was used to calculate the depth reliefs to the Moho boundary. The output map of the Moho relief and the corresponding crustal thickness were constructed for the Gulf of Aqaba. The depth from sea level down to the Moho discontinuity in the Gulf of Aqaba varies between about 37 km in the northern deep and abruptly changes to about 28 km at the southern area, Tiran Strait. Below the central part of the gulf, a Moho depth of about 34 km is obtained. The Red Sea crust is thinner than that of the Dead Sea rift; indicating the presence of a mantel upwelling that is related to the spreading of the sea floor. The asymmetry of crustal thickness between the eastern and western borders of the Gulf of Aqaba could be attributed to simultaneous strike-slip motion. The relative displacement between the two borders is observed clearly through the sea floor and Moho discontinuity. The displacement is nearly equivalent to 0.18° (i.e. about 20.4 km) and is assumed to be achieved in about 4.08 to 3.4 million years, according to the estimated rate of the transform motion along the Gulf of Aqaba (Dead Sea transform) that is about 0.5 to 0.6 cm/y.