Proceedings of the International School of Physics "Enrico Fermi.", Volume 78N. Zanichelli, 1953 - Nuclear physics |
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Page 362
... notion of continental drift - or at least the form of con- tinental drift which came to be called sea floor spreading [ 1 , 2 ] . This idea , and later refinements and elaborations of it , now serves as the guiding prin- ciple in terms ...
... notion of continental drift - or at least the form of con- tinental drift which came to be called sea floor spreading [ 1 , 2 ] . This idea , and later refinements and elaborations of it , now serves as the guiding prin- ciple in terms ...
Page 366
... notion that convection is confined to the upper mantle . On the basis of global distributions of seismicity such as discussed by ISACKS et al . [ 32 ] , it was recognized that the system of ridges and trenches , and their important ...
... notion that convection is confined to the upper mantle . On the basis of global distributions of seismicity such as discussed by ISACKS et al . [ 32 ] , it was recognized that the system of ridges and trenches , and their important ...
Page 440
... notion of mantlewide convection in a spherical shell whose inner radius / outer radius ratio , n , is 0.55 . Recent finite - amplitude studies by ZEBIB et al . [ 35 ] ( see fig . 34 in [ 1 ] ) on thermal convection in a base - heated ...
... notion of mantlewide convection in a spherical shell whose inner radius / outer radius ratio , n , is 0.55 . Recent finite - amplitude studies by ZEBIB et al . [ 35 ] ( see fig . 34 in [ 1 ] ) on thermal convection in a base - heated ...
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