Evaluation of the deformation parameters of the northern part of Egypt using Global Navigation Satellite System (GNSS)

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• 作者：Abdel-Monem S. Mohamed^a ; Ali M. Radwan^a ; ^{amradwaneg@yahoo.com" class="auth_mail" title="E-mail the corresponding author} ; Mohamed Sharf^b ; Zakaria Hamimi^b ; Esraa E. Hegazy^b ; Nadia Abou Aly^a ; Mahmoud Gomaa^a
• 关键词：Tectonic setting ; Crustal deformation ; Seismic activity ; Northern Egypt
• 刊名：NRIAG Journal of Astronomy and Geophysics
• 出版年：2016
• 出版时间：June 2016
• 年：2016
• 卷：5
• 期：1
• 页码：65-75
• 全文大小：3888 K

文摘

The northern part of Egypt is a rapidly growing development accompanied by the increased levels of standard living particularly in its urban areas. From tectonic and seismic point of views, the northern part of Egypt is one of the interested regions. It shows an active geologic structure attributed to the tectonic movements of the African and Eurasian plates from one side and the Arabian plate from the other side. From historical point of view and recent instrumental records, the northern part of Egypt is one of the seismo-active regions in Egypt. The investigations of the seismic events and their interpretations had led to evaluate the seismic hazard for disaster mitigation, for the safety of the densely populated regions and the vital projects. In addition to the monitoring of the seismic events, the most powerful technique of Global Navigation Satellite System (GNSS) will be used in determining crustal deformation where a geodetic network covers the northern part of Egypt. Joining the GPS Permanent stations of the northern part of Egypt with the Southern part of Europe will give a clear picture about the recent crustal deformation and the African plate velocity. The results from the data sets are compared and combined in order to determine the main characteristics of the deformation and hazard estimation for specified regions. Final compiled output from the seismological and geodetic analysis will throw lights upon the geodynamical regime of these seismo-active regions. This work will throw lights upon the geodynamical regime and to delineate the crustal stress and strain fields in the study region. This also enables to evaluate the active tectonics and surface deformation with their directions from repeated geodetic observations. The results show that the area under study suffers from continuous seismic activity related to the crustal movements taken place along trends of major faults