Abstract
We have relocated 259 inland earthquakes in northern Egypt using the double-difference hypocenter technique. Among this dataset we are able to determine source mechanisms of 200 events using P-wave polarities and amplitude ratios as well. The studied earthquakes have been recorded by the Egyptian National Seismological Network from October 1997 to December 2006 with local magnitude (ML) varies between 1.5 and 5.0. Three earthquake dislocations have been defined namely: Dahshour, southeast Beni-Suef, and Cairo-Suez district. Earthquake activities tend to occur in clusters along the first dislocation (Dahshour) however, relatively scattered along the second (southeast Beni-Suef) and the third (Cairo-Suez district) dislocations. At Dahshour dislocation three distinct clusters have been distinguished. Source mechanism solutions of Dahshour earthquakes displayed normal faulting with a strike-slip component to strike-slip faulting with a minor normal dip-slip component. Most of earthquake focal mechanism orientations are varying from NE-SW to NW-SE. The fault plane solutions of Beni-Suef earthquakes represented normal faulting with a strike-slip component. If the NNW-SSE striking plane has been chosen to be the actual fault plane, some solutions would indicated normal faulting with a sinistral strike-slip motion and other reflect normal faulting with a dextral strike-slip component. The fault plane solutions of Cairo-Suez district earthquakes are compatible with E-W to ENE-WSW striking normal fault with a dextral strike-slip motion.
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References
Abou Elenean KM (2007) Focal mechanisms of small and moderate size earthquakes recorded by the Egyptian National Seismic Network (ENSN), Egypt, NRIAG. J Geophys 6(1):119–153
Badawy A (1996) Seismicity and kinematic evolution of the Sinai plate. Ph D thesis, pp115, L. Eötvös Univ. Budapest
Badawy A (1998) Earthquake hazard analysis in northern Egypt. Acta Geod Geoph Hung 33(2–4):341–357
Badawy A (2001a) Status of the crustal stress as inferred from earthquake focal mechanisms and borehole breakouts in Egypt. Tectonophysics 343:49–61
Badawy A (2001b) The present-day stress field in Egypt. Ann Geofis 44(3):495–509
Badawy A (2005a) Seismicity of Egypt. Seismol Res Lett 76(2):149–161
Badawy A (2005b) Present-day seismicity, stress field and crustal deformation of Egypt. J Seismol 9(3):267–276
Badawy A, Abdel-Fattah AK (2001) Source parameters and fault plane determinations of the 28 December 1999 northeastern Cairo earthquakes. Tectonophysics 343(1–2):63–77
Badawy A, Horváth F (1999a) Recent stress field of the Sinai subplate region. Tectonophysics 304(4):385–403
Badawy A, Horváth F (1999b) Seismicity of the Sinai subplate region: kinematic implications. J Geodyn 27(4–5):451–468
Badawy A, Horváth F (1999c) Sinai subplate and kinematic evolution of the northern Red Sea. J Geodyn 27(4–5):433–450
Badawy A, Abdel-Monem SM, Abo-Ali N (2008a) Seismological and GPS constraints on the Sinai sub-plate motion along the Suez rift. Stud Geophys Geod 52(3):397–412
Badawy A, Abdel-Fattah AK, Ali SM, Farid W (2008b) Source parameters of the ML 4.1 earthquake of November 08, 2006, southeast Beni-Suef, northern Egypt. J Afr Earth Sci 51:151–159
Bosworth W, Steckler MR (1997) Stress field changes in the Afro-Arabian rift system during the Miocene to recent period. Tectonophysics 278:47–62
Bosworth W, Taviani M (1996) Late quaternary reorientation of stress field and extension direction in the southern Gulf of Suez, Egypt, evidence from uplifted coral terraces, mesoscopic fault arrays and borehole breakouts. Tectonics 5:791–802
Chen WP, Molnar P (1983) Focal depths of intracontinental and intraplate earthquakes and their implications for the thermal and mechanical properties of the lithosphere. J Geophys Res 88:4183–4214
Deichman N (1987) Focal depths of earthquakes in northern Switzerland. Ann Geophys B5:395–402
El-Hadidy S (1995) Crustal structure and its related causative tectonics in northern Egypt using geophysical data. Ph. D. Thesis, Ain Shams University
Halsey JH (1975) Interpretation of erts linears. Unpublished technical report. General Petroleum Company. Cairo, Egypt
Kebeasy RM (1990) Seismicity. In: Said R (ed) Geology of Egypt. A. A. Balkerma, Rotterdam, pp 51–59
Kebeasy R, Maamoun M, Albert R (1981) Earthquake activity and earthquake risk around the Alexandria area in Egypt. Acta Geophys Pol 29(1):37–48
Maggi A, Jackson JA, McKenzie D, Priestley K (2000) Earthquake focal depths, effective elastic thickness, and the strength of the continental lithosphere. Geology 28:495–598
Mahmoud S, Reilinger R, McClusky S, Vernant P, Tealeb A (2005) GPS evidence for northward motion of the Sinai block: implications for E. Mediterranean tectonics. Earth Planet Sci Lett 238:217–227
Meneisy MY (1990) Volcanicity. In: Said R (ed) The geology of Egypt, chapter 9. A.A. Balkema, Rotterdam, pp 157–172
Meshref WM (1982) Regional structural setting of northern Egypt. Proceeding of the 6th Egyptian general petroleum corporation exploration seminar, Cairo, pp 17–34
Moustafa A, Abd-Allah A (1992) Transfer zones with en echelon faulting at the northern end of the Suez rift. Tectonics 11(3):499–509. doi:10.1029/91TC03184
Moustafa A, El-Badrawy R, Gibali H (1998) Pervasive E-ENE oriented faults in northern Egypt and their effect on the Development and inversion of prolific sedimentary basis. Proceedings of 14th petroleum conference, vol 1. Egyptian General Petroleum Corporation, pp 51–67
Nelson R (1987) Notes on the northern termination of the Gulf of Suez rift into pre-existing E-W fault system. Petrology 24(11–12):57–62
Ranalli G, Murphy DC (1987) Rheological stratification of the lithosphere. Tectonophysics 132:281–295
Sibson RH (1982) Fault zone models, heat flow, and the depth distribution of earthquakes in the continental crust of the United States. Bull Seismol Soc Am 72:151–163
Snoke A (2003) Focal Mechanism determination software (FocMec package). http://www.geol.Vl.edu/outreach/focmec
Steckler M, Ten Brink U (1986) Lithosphere strength variations as a control on new plate boundaries: examples from the Northern Red Sea region. Earth Planet Sci Lett 79:120–132
Waldhauser F (2001) A program to compute Double-Difference Hypocenter Locations, US Geological survey, open-File Report, p. 01-113, Menlo park, CA
Waldhauser F, Ellsworth WL (2000) A double-difference earthquake location algorithm: method and application to the northern Hayward fault. Bull Seismol Soc Am 90:1353–1368
Acknowledgments
The authors are grateful to the Associate Editors Prof. Mariano Garcia-Fernandez and Prof. Steinunn Sigríður Jakobsdóttir and the two anonymous reviewers for their critical reviews which have greatly helped to improve the paper. This work has been carried out at Earthquake Division of the National Research Institute of Astronomy and Geophysics (NRIAG), the authors are also grateful to the all staff members of the ENSN.
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Badawy, A.A., AL-Werr, A. & Ali, S.M. Relative location and source mechanism of inland earthquakes in Northern Egypt. J Seismol 18, 257–276 (2014). https://doi.org/10.1007/s10950-013-9378-z
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DOI: https://doi.org/10.1007/s10950-013-9378-z