Distribution of energy in p and S Seismic bodily waves
DOI:
https://doi.org/10.54302/mausam.v17i3.5744Abstract
It is generally assumed that the energy in seismic bodily S waves is double that in the seismic bodily p waves. A theoretical explanation based on Debye's theory of specific heats o solids is suggested. The deduced result could also explain the observed fact that the wave frequency of p-waves is generally higher as compared to the wave frequency of S waves.
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