Articles | Volume 9, issue 4
Solid Earth, 9, 833–846, 2018
Solid Earth, 9, 833–846, 2018

Research article 06 Jul 2018

Research article | 06 Jul 2018

Density structure and isostasy of the lithosphere in Egypt and their relation to seismicity

Mikhail K. Kaban et al.

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Cited articles

Abdelwahed, M. F., El-Khrepy, S., and Qaddah, A.: Three-dimensional structure of the Conrad and Moho discontinuities in Egypt, J. Afr. Earth Sci., 85, 87–102, 2013.
Assumpção, M. and Sacek, V.: Intraplate seismicity and flexural stresses in central Brazil, Geophys. Res. Lett., 40, 487–491, 2013.
Azab, A., El-Khadragy, A., and Soliman, S. A.: Egyptian Crust: A structural model based on gravity and seismic data, J. Am. Sci., 11, 216–229, 2015.
Bosworth, W.: Geological evolution of the Red Sea: historical background, review, and synthesis, in: The Red Sea, 45–78, Springer Berlin Heidelberg, 2015.
Chen, B., Kaban, M. K., El Khrepy, S., and Al-Arifi, N.: Effective elastic thickness of the Arabian plate: Weak shield versus strong platform, Geophys. Res. Lett., 42, 3298–3304,, 2015.
Short summary
We present an integrative model of the crust and upper mantle of Egypt based on an analysis of gravity, seismic, and geological data. These results are essential for deciphering the link between the dynamic processes in the Earth system and near-surface processes (particularly earthquakes) that influence human habitat. We identified the distinct fragmentation of the lithosphere of Egypt in several blocks. This division is closely related to the seismicity patterns in this region.