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Acoustics of sedimentary/igneous section, Gulf of Aqaba coastal area, Egypt, and their applications to seismic hazards
Abd ElMaktader A. ElSayed

Dept. Geophysics, Fac. Sciences, Ain Shams Univ. Cairo, Egypt

Eighty five rock samples were collected from both sedimentary and igneous sections between Dahab and Taba, Gulf of Aqaba coastal area. Several petrophysical parameters were measured and calculated for some of the samples as: Porosity, density, velocities of elastic wave propagation, Piosson's ratio, Young's modules, bulk modules, rigidity, and specific acoustic impedance by which earthquake energy and seismic moment can be estimated.

Graphical plots have been constructed to throw light on the most reliable and applicable relationships for enhancing models used in seismic hazards studies. Vertical profiles of some measured petrophysical parameters show how much they are uniform and homogeneous as related to the sedimentary facies. Several linear models were calculated, characterized by high coefficient of correlation by which we can calculate a significant parameter from others which are usually measured during routine petrophysical analysis.

In the present work, shear wave velocity from the compressional wave velocity for both sedimentary and igneous sections can be calculated. In addition, using the apparent specific gravity considered as routine measurement, the rock rigidity, rock bulk modules and compressional wave velocity can also be estimated. The acoustic impedance can therefore be outlined with high accuracy from routine porosity measurements using the calculated linear model. The present work has its applications to seismic hazards and engineering constructions.