Titlebook: Seismic Ground Motion in Large Urban Areas; Giuliano F. Panza,Ivanka Paskaleva,Concettina Nunz Book 2004 Springer Basel AG 2004 Seismicity

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2504-3625 indings in ground-motion modeling, hazard prediction, risk a.The accelerated, and often uncontrolled, growth of the cities has contributed to the ecological transformation of their immediate surroundings. Factors contributing to the urban vulnerability include: lowering or rising of the water table,

Jubilation

Seismicity and Tectonic Structures in the Site of Algiers and its Surroundings: A Step Towards Micrarthquake catalogue is first made using all events reported in all previous documentation available. However for the sake of homogeneity and a certain degree of reliability of the data, only revised seismic events with epicenter coordinates, magnitude and/or intensity are included. A tectonic settin

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,Seismicity of Morocco for the Period 1987–1994,s registering magnitudes from 5 to 5.6. Such seismicity is particularly important for Morocco as the released seismic energy constitutes a considerable part of the total energy radiated during the 20th century. Relative seismicity maps confirm the persistence of the major features of the seismicity

Dorsal-Kyphosis

The Nile Valley of Egypt: A Major Active Graben that Magnifies Seismic Waves,all-to-moderate size earthquakes that have caused extremely severe damage to recent and historical constructions. The most vulnerable area along the Nile valley is the one of Cairo-Faiyoum. Small local and large distant earthquakes could be a source of huge socio-economic damage in this area. The lo

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Seismicity and Seismic Hazard in Alexandria (Egypt) and its Surroundings,of such damages is not well known. Seismogenic zones such as the Red Sea, Gulf of Aqaba-Dead Sea Hellenic Arc, Suez-Cairo-Alexandria, Eastern-Mediterranean-Cairo-Faiyoum and the Egyptian costal area are located in the vicinity of this city. The Egyptian coastal zone has the lowest seismicity, and th

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Ground Motion Zoning of Santiago de Cuba: An Approach by SH Waves Modelling,ms have been calculated along four profiles in the basin by the hybrid approach (modal summation for the path source-profile and finite differences for the profile) for a maximum frequency of 1 Hz. The response spectra ratio (RSR) has been determined in 49 sites, distributed along all considered pro

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Duration Magnitude Scale and Site Residuals for Northern Morocco,tained by relating the IGN (Instituto Geografico National, Madrid) body-waves mbLg. to the duration (τ), and the epicentral distance (Δ), at 25 analogue stations of the NMSNET for 479 earthquakes with 2.5 ≤ mb ≥ 5.4, from March 1992 to February 2001. .. estimates are significantly more precise while

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