Definition
The relationship of elastic longitudinal wave (Vp-waves) velocity to shear wave (Vs-waves) velocity or the relationship of elastic shear wave (Vs-waves) velocity to longitudinal wave (Vp-waves) velocity.
Characteristics
In engineering seismology, the velocity ratio Vp/Vs (TAU parameter) is considered as an indicator of the changes in stress state of rocks during the process of developing strong tectonic and volcanic earthquakes. It is well-known that deep fault zones, named gradiental zones, display rapid changes in the ratio Vp/Vs with a change of the anomalies’ sign (positive or negative). These can be considered as seismogenic zones. Relatively low values of Vp/Vs ratio indicate increases in activity in the magmatic chambers of volcanoes during their activization. The ratio of Vp-waves velocity to Vs-waves velocity (Vp/Vs) is used in engineering seismology and engineering geology (Slavina et al. 2015).
In engineering geology, the velocity ratios Vs/Vp and Vp/Vs аre used...
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References
Bondarev VI (1997) Seismic method of definition of physic-mechanical properties not rocky soils. USMGA, Ekaterinburg
Nikitin VN (1981) Bases of engineering seismicity. MSU, Moscow
Slavina LB, Kuchay MS, Lichodeev DV (2015) Assessment of kinematic parameter TAU behavior as indicator of the pressure variation on the example of the results of observations on Kamchatka and Caucasus. “Problems of complex geophysical monitoring of the Far East of Russia”. On 27th Sept – 3rd Oct 2015, Petropavlovsk-Kamchatsky
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Zhigalin, A. (2018). Velocity Ratio. In: Bobrowsky, P.T., Marker, B. (eds) Encyclopedia of Engineering Geology. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-73568-9_289
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DOI: https://doi.org/10.1007/978-3-319-73568-9_289
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