proof ch:13-continuum-elasticity@proof-26

open in the book · parts/03-classical-mechanics/13-continuum-elasticity.tex:1830

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proof : ch:13-continuum-elasticity@proof-26proofproposition 30.50: Love waves need a slow surface layer30.50definition 30.22: Boundary conditions of elastostatics30.22theorem 30.40: Navier–Cauchy equations30.40

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typedirectionnode provenancewhere
cites Some Problems of Geodynamics derived parts/03-classical-mechanics/13-continuum-elasticity.tex:1859
proves Love waves need a slow surface layer declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1830