proposition 30.50 Love waves need a slow surface layer

open in the book · parts/03-classical-mechanics/13-continuum-elasticity.tex:1811 · p. 1027

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proposition 30.50: Love waves need a slow surface layer30.50definition 30.22: Boundary conditions of elastostatics30.22theorem 30.40: Navier–Cauchy equations30.40proof : ch:13-continuum-elasticity@proof-26proofdefinition 10.24: Well-posed problem10.24theorem 30.21: Cauchy's equation of motion30.21proposition 30.48: Rayleigh's secular equation30.48proposition 30.23: Virtual work; the weak form30.23equation 30.21: eq:elast-hooke-isotropic30.21phenomenon 30.43: Two bulk wave speeds30.43proposition 30.41: Energy balance and its flux30.41remark 30.46: Why the plane-wave route, and not the potentials30.46proof : ch:13-continuum-elasticity@proof-18proof

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cites Some Problems of Geodynamics derived parts/03-classical-mechanics/13-continuum-elasticity.tex:1826
depends_on Boundary conditions of elastostatics declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1827
depends_on Navier–Cauchy equations declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1827
proves ch:13-continuum-elasticity@proof-26 declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1830