Proceedings of the International School of Physics "Enrico Fermi.", Volume 78N. Zanichelli, 1953 - Nuclear physics |
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Page 310
... curvature in the geotherm due to heat sources is insignificant in the mantle , where A = 4 nW / m3 . The continental geotherm proposed by STACEY [ 44 ] is generally higher than the others , and corresponds to a much higher surface heat ...
... curvature in the geotherm due to heat sources is insignificant in the mantle , where A = 4 nW / m3 . The continental geotherm proposed by STACEY [ 44 ] is generally higher than the others , and corresponds to a much higher surface heat ...
Page 418
... solution and it will be observed that the conduction profile has a 1/2 curvature rather than being linear as in the plane - layer case . This is simply a consequence of the fact that in steady state the total heat flow 418 W. R. PELTIER.
... solution and it will be observed that the conduction profile has a 1/2 curvature rather than being linear as in the plane - layer case . This is simply a consequence of the fact that in steady state the total heat flow 418 W. R. PELTIER.
Page 544
... curvature of the lithosphere in the Kuril Islands region . TURCOTTE et al . [ 45 ] extended the analysis by ... curvature of the trench - outer rise system requires several kbar bending stress as long as the thickness of the elastic ...
... curvature of the lithosphere in the Kuril Islands region . TURCOTTE et al . [ 45 ] extended the analysis by ... curvature of the trench - outer rise system requires several kbar bending stress as long as the thickness of the elastic ...
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