Seismic Hazards Implications of Uplifted Pleistocene Coral Terraces in the Gulf of Aqaba
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/s41598-017-00074-2.pdf
Reference71 articles.
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2. Bartov, Y., Steinitz, G., Eyal, M. & Eyal, Y. Sinistral movement along the Gulf of Aqaba: Its age and relation to opening the Red Sea. Nature 285, 220–221 (1980).
3. Garfunkel, Z. Internal structure of the Dead Sea leaky transform (rift) in relation to plate kinematics. Tectonophys 80, 81–108 (1981).
4. Eyal, M., Eyal, Y., Bartov, Y. & Steinitz, G. The tectonic development of the western margin of the Gulf of Elat (Aqaba) rift. Tectonophysics 80, 39–66 (1981).
5. Ben-Avraham, Z. Structural framework of the Gulf of Elat (Aqaba) northern Red Sea. J. Geophys. Res. 90, 703–726 (1985).
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