Anelasticity in the Earth by Frank D. Stacey, M. S. Paterson, A. Nicholas

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By Frank D. Stacey, M. S. Paterson, A. Nicholas

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Published through the yankee Geophysical Union as a part of the Geodynamics Series.

The indisputable fact that the fabrics within the reliable elements of the Earth go away from completely elastic behaviour is now critical to primary geophysical reviews. sluggish deformation (creep) by way of the procedures of mantle convection has been largely known for roughly 25 years; it's been realised much longer that seismic waves are attenuated yet extra lately there has built a basic if imprecise wisdom of a likely correlation among excessive attenuation and occasional resistance to creep and within the previous couple of years seismic attenuation has bought a lot better recognition since it implies a primary order dispersion of physique waves (frequency dependence of elasticity).


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Extra resources for Anelasticity in the Earth

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Anderson and H. Kanamori, Velocity dispersion due to anelasticity' implications for seismology and mantle composition, 41-58, 1976. Mitchell, B. , L. W. B. Leite, Y. K. Yu and Hermann, Attenuation of Love and Rayleigh waves across the Pacific at periods between 15 and 110 seconds, Bull. Seism. Soc. • 59, 427-444, 1969. Forsyth, D. , A new method for the analysis of multi-mode surface wave disperson' application of Love wave propagation in the East Pacific, Bull. Seism. Soc. , 65, 323-342, 1975.

For individual modes0S2-0S5, the measurementsare from the [1975] for Pacific Ocean paths for the period range 50 to ll0 seconds, are within a factor of 2 of our global average estimates. estimates for from (0S6-0S28), the measurements are from unsplit equal weight. coefficients rather normal modes; (2) Global mean group velocities (Figure 2) were calculated by averaging individual path Attenuation measurements Two types of measurements are included here: (1) for the period range 962-275 seconds for l) were formed for 20-second overlapping windows to produce averaged group velocity, as a function of period for each path.

Of models delineates our of attenuation within the mantle. set Modern digitally recording seismic stations, have made it feasible to collect and analyze data appropriate for quantitatively describing the average seismic wave attenuation within data to obtain models of the earth's seconds. Several different proaches have been taken to span this range of periods. Traveling surface * Present used. Such an inte- in detail. We then outline the data space inversion method, and the Q-1 models we have obtained.

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