Proceedings of the International School of Physics "Enrico Fermi.", Volume 78N. Zanichelli, 1953 - Nuclear physics |
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Page 321
... occur at the same time . The overall deformation rate of a solid is thus the sum of the two rates . For sufficiently low stresses diffusion creep ( or any other linear creep law ) dominates power law creep . At high stresses power law ...
... occur at the same time . The overall deformation rate of a solid is thus the sum of the two rates . For sufficiently low stresses diffusion creep ( or any other linear creep law ) dominates power law creep . At high stresses power law ...
Page 415
... occurs at high Rayleigh number . The geophysically relevant result of the calculations in [ 85 ] is that , with on ... occur , the magnitude of 7 must be sufficiently large to en- force a penetrative style of convection and the aspect ...
... occurs at high Rayleigh number . The geophysically relevant result of the calculations in [ 85 ] is that , with on ... occur , the magnitude of 7 must be sufficiently large to en- force a penetrative style of convection and the aspect ...
Page 474
... occurs catastrophically [ 50 ] , or a reduction in stress . We assigned the density contrasts to the sinking lithosphere ... occur during the time interval covered by the catalogue , either because the stresses in the slabs were not high ...
... occurs catastrophically [ 50 ] , or a reduction in stress . We assigned the density contrasts to the sinking lithosphere ... occur during the time interval covered by the catalogue , either because the stresses in the slabs were not high ...
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