Proceedings of the International School of Physics "Enrico Fermi.", Volume 78N. Zanichelli, 1953 - Nuclear physics |
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Page 168
... limit of low loss , provided that a few additional , less general , defi- nitions are adopted . The limit of low attenuation , or high Q , is characterized by small departure from elastic behavior , and thus is often amenable to treat ...
... limit of low loss , provided that a few additional , less general , defi- nitions are adopted . The limit of low attenuation , or high Q , is characterized by small departure from elastic behavior , and thus is often amenable to treat ...
Page 180
... limit of very large distance , the apparent signal velocity decreases to V1 = √M , / o , although this limit is very difficult to observe experimentally , since the wavefront degrades with propagation . = m In the limit a → 0 , Q ( w ) ...
... limit of very large distance , the apparent signal velocity decreases to V1 = √M , / o , although this limit is very difficult to observe experimentally , since the wavefront degrades with propagation . = m In the limit a → 0 , Q ( w ) ...
Page 560
... limit of transformation strain in a thin layer coinciding with S ; ET must be of order Au divided by the layer thickness , and hence become Dirac singular in the limit . In particular , if SV is some small volume element intersected by ...
... limit of transformation strain in a thin layer coinciding with S ; ET must be of order Au divided by the layer thickness , and hence become Dirac singular in the limit . In particular , if SV is some small volume element intersected by ...
Contents
B H HAGER and R J OCONNELL Lithospheric thickening | 1 |
Crustal deformation | 2 |
The piezomagnetic parameters | 3 |
Copyright | |
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adiabatic amplitude anelastic aspherical asthenosphere asymptotic attenuation body wave boundary conditions boundary layer calculations complex modulus constant convection corresponding crack creep crust D. L. ANDERSON defined deformation density dependence depth deviatoric diffusion discussed displacement distribution dynamic Earth model Earth Planet earthquake effect eigenfrequencies eigenfunctions elastic ellipticity energy equation estimate F. A. DAHLEN fluid free oscillations frequency Geophys GILBERT given gradient heat flow heat flux heat sources instability integral inverse problem J. R. Astron lateral heterogeneity linear solid lithosphere M₁ mantle convection measured mechanism modes modulus multiplet observed oceanic olivine parameters peak perturbation phase velocity Phys propagation radial Rayleigh number relaxation Rendiconti S.I.F. rheology rotation rupture scale sect seismic seismogram Seismol seismological shear shear stress shown in fig singlet slip solution spectra spectrum splitting strain stress drop structure surface waves temperature tensor theory thermal vector viscoelastic viscosity zone