Proceedings of the International School of Physics "Enrico Fermi.", Volume 78N. Zanichelli, 1953 - Nuclear physics |
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Page 178
... amplitude A ,. The ap- proximations made in deriving the scaling laws are only valid for frequencies and times ... amplitude , r amplitude Q Τα Τρ 60 d B Fig . 8 . -- T = t - tu Scaling parameters to characterize attenuated waveform ...
... amplitude A ,. The ap- proximations made in deriving the scaling laws are only valid for frequencies and times ... amplitude , r amplitude Q Τα Τρ 60 d B Fig . 8 . -- T = t - tu Scaling parameters to characterize attenuated waveform ...
Page 244
... amplitude . The rate of attenuation is related to the initial slope of the relaxation function . The PLS , on the other hand , has an infinite creep rate initially giving rise to a vanishing amplitude . The main wave for SLSCS ...
... amplitude . The rate of attenuation is related to the initial slope of the relaxation function . The PLS , on the other hand , has an infinite creep rate initially giving rise to a vanishing amplitude . The main wave for SLSCS ...
Page 452
... amplitude perturbations . The shaded area in fig . 10 reveals the possibility of finite - amplitude instability arising from sudden stress changes of a few bar . If these finite perturbations are maintained long enough at a total stress ...
... amplitude perturbations . The shaded area in fig . 10 reveals the possibility of finite - amplitude instability arising from sudden stress changes of a few bar . If these finite perturbations are maintained long enough at a total stress ...
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