Figure 8: Induced gravity load and residual gravity, Lake Nasser Area, Aswan, Egypt (from 2002 to 2004). Acknowledgements: The authors are in<strong>de</strong>bted to the Department of Geophysics, Faculty of Science, Cairo University and the National Research Institute of Astronomy and Geophysics (NRIAG) for the encouragement of this work. We thank the Regional Seismological Center at Aswan for providing the facilities for the measurements. Finally we are grateful to the German Aca<strong>de</strong>mic Exchange Service (DAAD) for supporting the work by travel funds to RMH and GJ. References Bell, M. L. and Nur, A., 1978. Strength changes due to reservoir - induced pressure and stress and application to Lake Oroville. J. Geophys. Res., vol. 83, pp. 4469 - 4483. Fat-Helbary, R. E., 1995. Assessment of seismic hazard and risk in Aswan area, Egypt. Ph. D. Thesis. Architectural Engineering Department Tokyo Univ., Japan, 182p. Hassan R.M., Ab<strong>de</strong>lrahman E.M., Tealeb A., Zahran K.H., Jentzsch G., 2009. Gravimetric ti<strong>de</strong> observation at Lake Nasser Region, Aswan, Egypt: a preliminary investigation, Bull. Inf. Marées Terrestres , 146, 11797-11806. Issawi, B., 1968. The geology of Kurkur - Dungle area. General Egyptian Organization for Geological Research and Mining, Geol. Surv. Cairo, Egypt. Paper No. 46, 102P. Issawi, B., 1978. Geology o f Nubia west area , Western Desert, Egypt. Annals Geo. Surv., Egypt, vol. 8, PP. 237 – 253. Kebeasy, R. M. Maamoun, M. and Ibrahim, E., 1982. Aswan Lake induced earthquakes. Bull. Int. Inst. Seismology & Earthquake Engineering, Tokyo, Japan, vol. 19. Kebeasy, R. M., Maamoun, M., Ibrahim, E. M., Meghahed, A., Simpson, D. and Leith, W., 1987. Earthquake studies at Aswan reservoir. J. of Geodynamics, Vol. 7, pp. 173–197. Roeloffs, E. A., 1988. Fault stability changes induced beneath a reservoir with cyclic variations in water level. J. Geophys. Res., vol. 93, pp. 2107-2124. Snow, D. T., 1972. Geodynamic of seismic reservoirs, symposium on perco<strong>la</strong>tion through fissured rocks. Proceedings, Deutsche Gesellschaft für Erd- und Grundbau, Germany, T2- J, pp. 1- 14. Simpson, D. W., 1986. Triggered Earthquakes. Ann. Rev. Earth p<strong>la</strong>nt Sci. 14, 21- 42. Vyskočil, P. and Tealeb, A., 1985. Report on activity by monitoring recent crustal movement at Aswan period 1983-1985. Bull. Helwan Inst. of Astronomy and Geoph., vol. II, Ser. B, pp. 33-41. Vyskočil, P., 1987. Recommendations on the project of monitoring recent crustal movements in the western part of the Aswan region in Egypt. J. of Geodynamics, vol.7, pp. 257-259. 11816
Vyskočil, P. and Tealeb, A., 1995. The present stage and prospect for recent crustal movement studies around seismo-active areas in Egypt. Bull. Helwan Inst. of Astronomy and Geophysics, vol. xi, pp. 105-138. Wenzel, H. G., 1996a. The nanogal software: Earth ti<strong>de</strong> data processing package ETERNA 3.30. Bulletin d’Inf. Marèes Terr., vol. 124, pp. 9425-9439. Wenzel, H. G., 1997. Analysis of the Earth ti<strong>de</strong> observations In: Wilhelm, H., W. Zürn and H.-G. Wenzel (Eds), Tidal Phenomena. Lecture Notes in Earth Sciences, Springer Ver<strong>la</strong>g, Berlin, Germany, pp. 59-75. WCC (Woodward - Cly<strong>de</strong> Consultants), 1985. I<strong>de</strong>ntification of earthquake sources and estimation of magnitu<strong>de</strong>s and recurrence intervals, Internal Report, High and Aswan Dams Authority, Aswan, Egypt, 135p. Zhang, K. F., Featherstone, W. E. , Bian, S. F., and Tao, B. Z., 1996. Time variation of the Earth's gravity field and crustal <strong>de</strong>formation due to the establishment of the Three Gorges reservoir, J. Geod., vol. 70, pp. 440-449. Zahran, K. H., Jentzsch, G. and Seeber, G., 2005. World – wi<strong>de</strong> synthetic ti<strong>de</strong> parameters for gravity and vertical and horizontal disp<strong>la</strong>cements. J. Geod., vol. 79, pp. 293-299. Zahran, K. H., 2005. Benefit of tidal observations to gravity and GPS networks. Egyptian Geophys. Soc. Journal, vol. 3, No. 1, pp 89-98. 11817
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1994), and TPXO.6 (Egbert et al., 1
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From Fig. 2, we also see that, the
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GPS network called GEONET (GPS Eart
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References Bos, M. S., Baker, T. F.
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Planets Space, 59, 307-311. Sato, T
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Fig. 1. Locations of the observatio
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