Proceedings of the International School of Physics "Enrico Fermi.", Volume 78N. Zanichelli, 1953 - Nuclear physics |
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Page 417
... increase of not much more than one order of magnitude . Such an increase will probably allow us to re- concile both the free - air and sea - level data , but would be completely insuf- ficient to inhibit whole - mantle convection . This ...
... increase of not much more than one order of magnitude . Such an increase will probably allow us to re- concile both the free - air and sea - level data , but would be completely insuf- ficient to inhibit whole - mantle convection . This ...
Page 424
... increase . From ( 62c ) this causes the Nusselt number to increase and from ( 62b ) the heat flux will likewise increase and thus also the rate of cooling which will then act contrary to the original tendency . The opposite reaction ...
... increase . From ( 62c ) this causes the Nusselt number to increase and from ( 62b ) the heat flux will likewise increase and thus also the rate of cooling which will then act contrary to the original tendency . The opposite reaction ...
Page 427
... increase of the creep activation energy and therefore an in- crease of viscosity . Some increase of viscosity at this depth also seems neces- sary to reconcile the magnitude of the observed free - air gravity anomaly over the Canadian ...
... increase of the creep activation energy and therefore an in- crease of viscosity . Some increase of viscosity at this depth also seems neces- sary to reconcile the magnitude of the observed free - air gravity anomaly over the Canadian ...
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