Proceedings of the International School of Physics "Enrico Fermi.", Volume 78N. Zanichelli, 1953 - Nuclear physics |
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Page 349
... effect of thermal vibrations is to << soften the material , i.e. the bulk modulus is decreased by the thermal - pres- sure term . This effect increases with q and decreases with compression . The converse is valid for all q values ...
... effect of thermal vibrations is to << soften the material , i.e. the bulk modulus is decreased by the thermal - pres- sure term . This effect increases with q and decreases with compression . The converse is valid for all q values ...
Page 521
... effects give « sinks » of entropy . The « sources » come from dissipative processes like Ohmic and viscous heating , but the most important effect is thermal conduction . All of these effects are positive definite . Some heat is ...
... effects give « sinks » of entropy . The « sources » come from dissipative processes like Ohmic and viscous heating , but the most important effect is thermal conduction . All of these effects are positive definite . Some heat is ...
Page 628
... effects are similar in kind to the analogous effects due to Biot elastic response as discus- sed in subsect . 8'3 and 8'4 . - 86. Dilatancy effects during the slip - weakening process in shear crack prop- agation . To examine the effect ...
... effects are similar in kind to the analogous effects due to Biot elastic response as discus- sed in subsect . 8'3 and 8'4 . - 86. Dilatancy effects during the slip - weakening process in shear crack prop- agation . To examine the effect ...
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