phenomenon 30.43 Two bulk wave speeds

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phenomenon 30.43: Two bulk wave speeds30.43proposition 30.30: Stability bounds30.30theorem 30.40: Navier–Cauchy equations30.40phenomenon 30.47: The three seismic phases30.47remark 30.46: Why the plane-wave route, and not the potentials30.46proof : ch:13-continuum-elasticity@proof-21proofequation 30.23: eq:elast-energy-density30.23theorem 5.116: Sylvester's law of inertia5.116phenomenon 30.32: Poisson contraction30.32proposition 30.34: Minimum of the potential energy30.34theorem 30.42: Uniqueness in elastodynamics30.42proof : ch:13-continuum-elasticity@proof-13proofequation 30.21: eq:elast-hooke-isotropic30.21theorem 30.21: Cauchy's equation of motion30.21proposition 30.41: Energy balance and its flux30.41proposition 30.50: Love waves need a slow surface layer30.50proposition 30.48: Rayleigh's secular equation30.48proof : ch:13-continuum-elasticity@proof-18proofproposition 30.49: The Rayleigh speed of a Poisson solid30.49proof : ch:13-continuum-elasticity@proof-23prooftheorem 7.137: Helmholtz decomposition7.137

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cites On the propagation of earthquake motion to great distances derived parts/03-classical-mechanics/13-continuum-elasticity.tex:1459
cites Mémoire sur l'équilibre et le mouvement des corps élastiques derived parts/03-classical-mechanics/13-continuum-elasticity.tex:1457
depends_on Stability bounds declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1461
depends_on Navier–Cauchy equations declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1461
depends_on The three seismic phases declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1624
depends_on Why the plane-wave route, and not the potentials declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1604
proves ch:13-continuum-elasticity@proof-21 declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1464