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Most elastic waves recorded close to an extended fault source are complicated and difficult to interpret uniquely.
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The proposed concept is based on the ability of most periodic structures to forbid elastic waves from propagating within specific frequency ranges known as phononic bandgaps.
Generals lament a military stretched beyond its most elastic means.
Elastic waves of various types radiate from the vicinity of the moving rupture in all directions.
Earthquakes generate four principal types of elastic waves; two, known as body waves, travel within the Earth, whereas the other two, called surface waves, travel along its surface.
By not even the most elastic stretch of the imagination was this a gingerbread house.
These are called shock waves; they can propagate much beyond the speed of linear elastic waves and are accompanied by significant heating.
During the reaction, Dobson's team measured elastic waves analogous to the seismic waves that shake Earth's crust.
Researchers have also developed materials that can cloak objects against sound waves, ocean waves, and even the elastic waves in Earth's crust caused by earthquakes.
Elastic waves couple with light through the acousto-optic interaction.
For simplicity, we here consider formulations for elastic waves without anelastic attenuation to explain the scheme.
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