Proceedings of the International School of Physics "Enrico Fermi.", Volume 78N. Zanichelli, 1953 - Nuclear physics |
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Results 1-3 of 75
Page 139
... results : Result 1 : ( 3.35 ) N ( a ) ( 2 ) v ( a , 8 ( 2 ) = 0 ( a = 1,2 ; B = = 1 , 2 ) . Result 2 : ( 3.36 ) N ( a ) 2 ( 2 ) = 0 ( α = 1 , 2 ) . Result 3 : ( 3.37 ) ΣΝ ( α ) ( 2 ) = N ( a ) ( z ) Σ , Να ' Σ = ΣΝ ( α ) ( α = = 1 , 2 ) .
... results : Result 1 : ( 3.35 ) N ( a ) ( 2 ) v ( a , 8 ( 2 ) = 0 ( a = 1,2 ; B = = 1 , 2 ) . Result 2 : ( 3.36 ) N ( a ) 2 ( 2 ) = 0 ( α = 1 , 2 ) . Result 3 : ( 3.37 ) ΣΝ ( α ) ( 2 ) = N ( a ) ( z ) Σ , Να ' Σ = ΣΝ ( α ) ( α = = 1 , 2 ) .
Page 142
... results of sect . 3 we now show : Result 9 : When w , k are such that 4 ( w , k ) = function ( 2 ) such that = 0 , there exists an eigen- N1 ( 2 ) P ( z , 26 ) N ( 2 ) ( ≈。) Σ = — N ( 2 ) ( z ) P ( z , ≈0 ) N ( 1 ) ( ≈0 ) Σ = p ( z ) ...
... results of sect . 3 we now show : Result 9 : When w , k are such that 4 ( w , k ) = function ( 2 ) such that = 0 , there exists an eigen- N1 ( 2 ) P ( z , 26 ) N ( 2 ) ( ≈。) Σ = — N ( 2 ) ( z ) P ( z , ≈0 ) N ( 1 ) ( ≈0 ) Σ = p ( z ) ...
Page 143
... result 9. It may be noted that the first equality in ( 4.5 ) ensures that the contribution from each mode is continuous at the source . A similar result may be obtained for the branch cut contributions in ( 4.1 ) and we shall now show ...
... result 9. It may be noted that the first equality in ( 4.5 ) ensures that the contribution from each mode is continuous at the source . A similar result may be obtained for the branch cut contributions in ( 4.1 ) and we shall now show ...
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