remark 30.46 Why the plane-wave route, and not the potentials

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remark 30.46: Why the plane-wave route, and not the potentials30.46phenomenon 30.43: Two bulk wave speeds30.43theorem 7.137: Helmholtz decomposition7.137theorem 30.40: Navier–Cauchy equations30.40proposition 30.30: Stability bounds30.30phenomenon 30.47: The three seismic phases30.47proof : ch:13-continuum-elasticity@proof-21proofproposition 7.123: Second-order identities of the nabla calculus7.123proposition 10.67: The Newtonian potential is the fundamental solution10.67theorem 7.109: Leibniz integral rule7.109remark A.527: The hypotheses, and what happens without themA.527remark 30.27: Two results this chapter borrows from Part II30.27remark 10.73: What compact support is doing, and the rate that replaces it10.73remark 10.74: Where the decomposition is used, and what it costs10.74proof : app:A-long-proofs@proof-317proofproof : ch:05-real-analysis@prooflink-4proofequation 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-18proof

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depends_on Two bulk wave speeds declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1604
depends_on Helmholtz decomposition declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1604
depends_on Navier–Cauchy equations declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1604