Proceedings of the International School of Physics "Enrico Fermi.", Volume 78N. Zanichelli, 1953 - Nuclear physics |
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Page 112
... contribution to s ( r , t ) of surface wave energy propagating along paths other than P is small . Seen from this surface wave viewpoint , the two results ( 80 ) and ( 84 ) seem intuitively quite reasonable . From a strictly normal ...
... contribution to s ( r , t ) of surface wave energy propagating along paths other than P is small . Seen from this surface wave viewpoint , the two results ( 80 ) and ( 84 ) seem intuitively quite reasonable . From a strictly normal ...
Page 127
... contribution , since the evaluation of the SH component does not present the same difficulties . The intergrand for the P - SV contribution involves the solution of a boundary- value problem posed in terms of a stress - displacement ...
... contribution , since the evaluation of the SH component does not present the same difficulties . The intergrand for the P - SV contribution involves the solution of a boundary- value problem posed in terms of a stress - displacement ...
Page 349
... contribution of the thermal vibrations to the bulk modulus at any tem- perature and at any compression . In other words , it implies that the elastic properties of the solid are totally unaffected by temperature and its use is ...
... contribution of the thermal vibrations to the bulk modulus at any tem- perature and at any compression . In other words , it implies that the elastic properties of the solid are totally unaffected by temperature and its use is ...
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