Proceedings of the International School of Physics "Enrico Fermi.", Volume 78N. Zanichelli, 1953 - Nuclear physics |
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Page 105
... decay rate a , and its own excitation amplitude A , ( r ) ; the latter depend on the source parameters r , and M. The decay rates a , are related to singlet quality factors Q , by a , w , / 2Q ,. In the time domain , the signal ...
... decay rate a , and its own excitation amplitude A , ( r ) ; the latter depend on the source parameters r , and M. The decay rates a , are related to singlet quality factors Q , by a , w , / 2Q ,. In the time domain , the signal ...
Page 326
... decay of stress in a non - Newtonian Maxwell substance ( power law n ) which was strained by an amount & at t = 0 and held fixed thereafter ( eq . ( 18 ) ) . Note the dependence of decay rate upon the power n after one Maxwell time has ...
... decay of stress in a non - Newtonian Maxwell substance ( power law n ) which was strained by an amount & at t = 0 and held fixed thereafter ( eq . ( 18 ) ) . Note the dependence of decay rate upon the power n after one Maxwell time has ...
Page 517
... decays to 26Mg with a half - life of 0.74 My and would remain a significant source of heat for about 10 My . If the Earth accreted within 20 My of the termination of nucleosynthesis , the heat released through the decay of 26 Al could ...
... decays to 26Mg with a half - life of 0.74 My and would remain a significant source of heat for about 10 My . If the Earth accreted within 20 My of the termination of nucleosynthesis , the heat released through the decay of 26 Al could ...
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