Proceedings of the International School of Physics "Enrico Fermi.", Volume 78N. Zanichelli, 1953 - Nuclear physics |
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Page 15
... considered by introducing other weigh- ting functions . = 3'11 . Various linear operations mapping M onto itself can be defined : projection , smoothing , etc. For example , the computation of the radial part of Am can be denoted by Am ...
... considered by introducing other weigh- ting functions . = 3'11 . Various linear operations mapping M onto itself can be defined : projection , smoothing , etc. For example , the computation of the radial part of Am can be denoted by Am ...
Page 595
... considered . Also , eq . ( 5.21 ) applies for K if D is replaced by D / f . These results are used ( with a → ∞ ) in subsect . 6'3 for an asymptotic analysis of dynamic crack growth with a small slip - weakening zone . 6 . - Slip ...
... considered . Also , eq . ( 5.21 ) applies for K if D is replaced by D / f . These results are used ( with a → ∞ ) in subsect . 6'3 for an asymptotic analysis of dynamic crack growth with a small slip - weakening zone . 6 . - Slip ...
Page 655
... considered , inter- spersed in an inert rock matrix with a volume ratio q , the overall piezomagnetic coefficients can be computed as average values over all possible crystal orientations [ 14 ] ( 30 ) 27 2л +1 զ < Qisk > = 8л2 Saç fdy ...
... considered , inter- spersed in an inert rock matrix with a volume ratio q , the overall piezomagnetic coefficients can be computed as average values over all possible crystal orientations [ 14 ] ( 30 ) 27 2л +1 զ < Qisk > = 8л2 Saç fdy ...
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