Proceedings of the International School of Physics "Enrico Fermi.", Volume 78N. Zanichelli, 1953 - Nuclear physics |
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Page 519
... gravitational energy as a result of the concentration of the high - density nickel - iron in the centre of the Earth . TOZER [ 44 ] estimated the increase of heat arising from core formation from an originally undifferentiated Earth to ...
... gravitational energy as a result of the concentration of the high - density nickel - iron in the centre of the Earth . TOZER [ 44 ] estimated the increase of heat arising from core formation from an originally undifferentiated Earth to ...
Page 527
... gravitational energy , 20 per cent from cooling , 5 per cent from chemical internal energy and 1 per cent from adiabatic heating . On the other hand , the entropy available for dissipation comprises 67 per cent gravitational , 25 per ...
... gravitational energy , 20 per cent from cooling , 5 per cent from chemical internal energy and 1 per cent from adiabatic heating . On the other hand , the entropy available for dissipation comprises 67 per cent gravitational , 25 per ...
Page 546
... gravitational pull of dense subducted slab at island arcs [ 58 ] , 2 ) gravitational sliding or pushing from ocean ridges [ 59 ] , 3 ) viscous drag due to the convection current in the asthenosphere . The forces that resist plate ...
... gravitational pull of dense subducted slab at island arcs [ 58 ] , 2 ) gravitational sliding or pushing from ocean ridges [ 59 ] , 3 ) viscous drag due to the convection current in the asthenosphere . The forces that resist plate ...
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