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A Panel diagram shows subsurface geologic depth model for a part of the study area from the boreholes where the surface elevation is illustrated by contour lines and the location of the seismic profiles and the drilled wells are illustrated. Locations of the correlated boreholes are shown in Figure 2. 

A Panel diagram shows subsurface geologic depth model for a part of the study area from the boreholes where the surface elevation is illustrated by contour lines and the location of the seismic profiles and the drilled wells are illustrated. Locations of the correlated boreholes are shown in Figure 2. 

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Determination of the dynamic geotechnical properties and Vs30 of soil and rocks from seismic wave velocities serves as essential inputs for a foundation design cognizant of seismic site response and rock strength. This study evaluates a site which was suggested for a Nuclear Power Plant (NPP) in El-Dabaa area, north western coast of Egypt. On the n...

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Context 1
... composed mainly of limestone of different ages from Pleistocene to Miocene in the south. These ridges are cut with wadis filled with loamy deposits, except between the first ridge (in the north) and second ridge the wadis were filled by Sabkha (lagoon) deposits (Fig. 2), [4,5]. The shallow subsurface succession in the study area is illustrated in Fig. ...
Context 2
... boreholes findings with good depth agreement. The correlation illustrate that the three layers obtained from the seismic models more or less equivalent to the boreholes models in the surface and the third layer (oolitic limestone) but the intermediate layer in the seismic models is classified into two or more thin beds in the boreholes models (Fig. ...
Context 3
... ridges are cut with wadis filled with loamy deposits, except between the first ridge (in the north) and second ridge the wadi filled by Sabkha (lagoon) deposits (Fig.3), (Abu El Ella, 1987, 1992). The shallow subsurface succession in the study area is illustrated in Figure 4. ...
Context 4
... models from seismic profiles were correlated with the drilled boreholes findings with good depth agreement. The correlation illustrate that the three layers obtained from the seismic models more or less equivalent to the boreholes models in the surface and the third layer (oolitic limestone) but the intermediate layer in the seismic models is classified into two or more thin beds in the boreholes models (Fig.4) (Figs.7 and 8). ...

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... Low-cost noninvasive geophysical methods have recently proven their effectiveness in resolving targets related to engineering problems. Geophysical methods such as seismic refraction, multi-channel analysis of surface wave (MASW), ground penetrating radar (GPR) and geoelectrical methods have long been used to delineate shallow features of interest in engineering applications (e.g., Ballard and Mclean 1975;Sharma 1997;Rucker and Holmquist 2006;Rucker and Fergason 2006;Al-Saigh and Al-Heety 2013;Shaaban et al. 2013;Ólafsdóttir 2016;Abudeif et al. 2017;Adewoyin et al. 2017;Pilecki et al. 2017;Karabulut 2018;Allo et al. 2019;Butchibabu et al. 2019). The seismic refraction method is a common low-cost geophysical technique to investigate the subsurface and is characterized by its high efficiency for shallow target investigations (Hatherly 1982;Lankston 1990;Sheriff and Geldart 1995;Palmer 2001;Palmer et al. 2005;Whiteley and Eccleston 2006;Zhigulev and Patrikeev 2007;Sloan et al. 2015;Brixová et al. 2018). ...
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