phenomenon 30.47 The three seismic phases

open in the book · parts/03-classical-mechanics/13-continuum-elasticity.tex:1610 · p. 1025

Rests on

Supports

Nothing declares a dependency on this node yet.

Neighborhood

Every logical edge within two steps of this node.

phenomenon 30.47: The three seismic phases30.47phenomenon 30.43: Two bulk wave speeds30.43proposition 30.49: The Rayleigh speed of a Poisson solid30.49proof : ch:13-continuum-elasticity@proof-23proofproposition 30.30: Stability bounds30.30theorem 30.40: Navier–Cauchy equations30.40remark 30.46: Why the plane-wave route, and not the potentials30.46proof : ch:13-continuum-elasticity@proof-21proofproposition 30.48: Rayleigh's secular equation30.48proof : ch:13-continuum-elasticity@proof-25proof

Edges

typedirectionnode provenancewhere
cites Some Problems of Geodynamics derived parts/03-classical-mechanics/13-continuum-elasticity.tex:1623
cites On the propagation of earthquake motion to great distances derived parts/03-classical-mechanics/13-continuum-elasticity.tex:1616
cites On Waves Propagated along the Plane Surface of an Elastic Solid derived parts/03-classical-mechanics/13-continuum-elasticity.tex:1621
depends_on Two bulk wave speeds declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1624
depends_on The Rayleigh speed of a Poisson solid declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1624
proves ch:13-continuum-elasticity@proof-23 declared parts/03-classical-mechanics/13-continuum-elasticity.tex:1627