PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Earthquake hazard analysis in Alexandria, Egypt

Autorzy
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Alexandria , as a second major city of Egypt, becomes nowadays a site for new developmental projects. Therefore, the seismic hazard analysis would be essential to mitigate the earthquake disaster in the region. The seismic hazard maps of different non-exceedence probability for Alexandria are presented. The obtained results indicate that Alexandria is highly affected by earthquakes are generated north of Red Sea and its two branches (Gulf of Suez and Gulf of Aqaba). Recently, the southwest Cairo (Dahshour district) is reported as a source region and poses an effect on the new constructions in Alexandria. Detailed seismic hazard estimation has been carried out for three important constructions: Alexandria Library, Stanley Bridge and the fort of Qaitbay (old Alexandria lighthouse). At the three sites, four intensity levels have been examined. The annual expected number of earthquake, the return period, and the probability of occurrence were calculated for each intensity level. The obtained results indicate that the return period of intensity 5.0 for the Alexandria Library and Stanley Bridge is about 47 years with 2.0% probability of occurrence. Thus, Alexandria Is and area of moderate seismic hazard.
Rocznik
Strony
387--398
Opis fizyczny
Bibliogr. 13 poz.
Twórcy
autor
  • Physics Department, Faculty of Science Alexandria University, Alexandria, Egypt
Bibliografia
  • 1. Ambraseys, N.N., C.P. Melville and R.D. Adam, 1994, The seismicity of Egypt, Arabia and Red sea: a historical review, Cambridge University Press, Cambridge.
  • 2. Badawy, A., 1996, Seismicity and kinematic evolution of the Sinai plate, Ph. D. thesis, L. Eotvos Univ. Budapest, pp. 115.
  • 3. Badawy, A., 1998, Earthquake hazard analysis in northern Egypt, Acta Geod. Geoph. Hung. 33,2-4,341-357.
  • 4. Badawy , A., 1999, Historical seismicity of Egypt, Acta Geod. Geoph. Hung. 34, 1-2, 119-135.
  • 5. Badawy, A., 2001, Status of the crustal stress as inferred from earthquake focal mechanism and borehole breakout in Egypt, Tectonophysics 343, 1-2, 49-61.
  • 6. Badawy, A., and F. Horváth, 1999a, Seismicity of the Sinai sub plate region: Kinematic implications, J. Geodynamics 27, 4-5, 451-468.
  • 7. Badawy, A., and F. Horváth, 1999b, Sinai sub plate and kinematic evolution of the northern Red Sea, J. Geodynamics 27,4-5, 433-450.
  • 8. El-Araby, H., and M. Sultan, 2000, Integrated seismic risk map of Egypt, Seism. Res. Letten 71, 53-66.
  • 9. El-Sayed, A., F. Vaccari and G.F. Panza, 2001, Deterministic seismic hazard in Egypt, Geophys. J. Inter. 144, 555-567.
  • 10. Kebeasy, R., 1990, Seismicity. In: R. Said (ed.), "Geology of Egypt", Balkema, Rotterdam, 51-59.
  • 11. Maamoun, M., 1979, Observed intensity-epicentral distance relations in Egyptian earthquakes Bull. Helwan Observ. 184, 12 p.
  • 12. Mogi, K., 1962, Study of elastic shocks caused by fracture of heterogenous materials and it Relations to earthquake phenomena, Bull. Earthq. Res. Inst. Tokyo 40, 125-173.
  • 13. Scholz, C.H., 1968, The frequency-magnitude relation of microfracturing and its relation earthquakes, B.S.S.A. 58, 399-417.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0007-0054
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.