Proceedings of the International School of Physics "Enrico Fermi.", Volume 78N. Zanichelli, 1953 - Nuclear physics |
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Page 31
... curve . BACKUS and GIL- BERT [ 70 ] have demonstrated that this curve has a number of interesting prop- erties . In particular , for points on the tradeoff curve , decreasing o always increases : an increase in the d - ness of an ...
... curve . BACKUS and GIL- BERT [ 70 ] have demonstrated that this curve has a number of interesting prop- erties . In particular , for points on the tradeoff curve , decreasing o always increases : an increase in the d - ness of an ...
Page 177
... curve a ) t = 150 s , curve b ) t = 200 s , curve c ) t1 = 400 s , curve d ) t 600 s , curve e ) t = 800 s , curve f ) t1 = 1000 s . Q is con- ΤΗ = = stant in the band [ Tm , Ty ] , t is unrelaxed travel time . From [ 26 ] . 12 ...
... curve a ) t = 150 s , curve b ) t = 200 s , curve c ) t1 = 400 s , curve d ) t 600 s , curve e ) t = 800 s , curve f ) t1 = 1000 s . Q is con- ΤΗ = = stant in the band [ Tm , Ty ] , t is unrelaxed travel time . From [ 26 ] . 12 ...
Page 375
... curve from the 14C dates for the Richmond Gulf beaches compared with a theoretical calculation ( solid curve ) . The data are from ref . [ 49 ] . sequence can be determined using radiocarbon dating and , if the height of each horizon ...
... curve from the 14C dates for the Richmond Gulf beaches compared with a theoretical calculation ( solid curve ) . The data are from ref . [ 49 ] . sequence can be determined using radiocarbon dating and , if the height of each horizon ...
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