Abstract
The mechanisms contributing to the attenuation of earthquake ground motion in the distance range of 10 to 200 km are studied with the aid of laboratory data, coda waves and strong motion attenuation measurements in northeast United States and Canada and theoretical models. The relative contributions to attenuation of anelasticity of crustal rocks (constant Q), fluid flow and scattering are evaluated. Scattering is found to be strong with albedo of B0=0.9 and scattering extinction length of about 17 km. The intrinsic attenuation in the crust can be explained by a high constant Q(500 ≤ Q0 ≤ 2000) and a frequency dependent mechanism most likely due to fluid effects in rocks and cracks. A fluid-flow attenuation model gives a frequency dependence (Q ≃ Q0 f0.5) similar to those determined from the analysis of coda waves of regional seismograms.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Aki, K., and Chouet, B.,(1975),Origin of coda waves: source, attenuation and scattering effects, J.Geophys. Res., 80, 3322–3342.
Aki, K.,(1980),Attenuation of shear waves in the lithosphere for frequencies from 0.05 to 25 Hz, Phys. Earth Planet. Inter., 21, 50–60.
Aki, K., and Richards, P.G.,(1980),Quantitative seismology. Theory and methods. W.H. Freeman and Co., San Francisco.
Auriault, J.L., Borne, L., and Chambon, R.,(1985),Dynamics of porous saturated media,; checking of the generalized law of Darcy, J.Acoust.Soc. Am., 77, 1641–1650.
Birch, F., and Bancroft, D.,(1938),Elasticity and internal friction in a long column of granite, Bull. Seism. Soc. Am., 28, 243–254.
Bradley, J.J., and Fort, A.N.Jr.,(1966),Internal friction in rocks in Handbook of Physical constants, S.P.Clark, Jr., Ed., GSA Publ., p.175–193.
Brown, R.J.S., and Korringa, J.,(1975),On the dependence of the elastic properties of a porous rock on the compressibility of the pore fluid, Geophysics, 40, 608–616.
Biot, M.A.,(1956a),Theory of propagation of elastic waves in a fluid saturated porous solid. I.Low frequency range, J.Acoust. Soc.Am., 28, 168–178.
Biot, M.A.,(1956b),Theory of propagation of elastic waves in a fluid saturated porous solid. II.Higher frequency range, J.Acoust. Soc. Am., 28, 179–191.
Biot, M.A.,(1962), Mechanics of deformation and acoustic propagation in porous media, J.Appl. Phys., 33, 1482–1488.
Clark, V.A., Spencer, T.W., Tittmann, B.R., Ahlberg, L.A., and Coombe, L.T.,(1980),Effect of volatiles on attenuation Q-1 and velocity in sedimentary rocks, J.Geophys. Res., 85, 5190–5198.
Dainty, A.M., Goins, N.R., and Toksöz,M.N.,(1976),Seismic investigation of the lunar interior, in Lunar science VII:Houston Lunar Science Institute, p.181–183.
Dainty, A.M., and Toksöz,M.N.,(1977),Elastic wave propagation in a highly scattering medium. A diffusion approach, J.Geophys., 43, 375–388.
Dainty, A.M., and Tóksöz,M.N.,(1981),Seismic codas on the Earth and the Moon: a comparison, Phys. Earth and Plan. Int., 26, 250–260.
Dunn, K.J.,(1985),Acoustic attenuation in fluid saturated porous cylinders at low frequencies, J.Acoust.Soc.Am, 79, 1709–1721.
Gao, L.S., Lee, L.C., Biswas, N.H., and c, K.,(1983a),Comparison of the effects between single and multiple scattering on coda waves for local earthquakes, Bull.Seism. Soc. Am., 73, 373–389.
Gao, L.S., Lee, L.C., Biswas, N.H., and Aki, K.,(1983b),Effects of multiple scattering on coda waves in three-dimensional medium, Pure and Applied Geoph., 121, 3–15.
Gardner, G.H.F., Wyllie, M.R.J., and Droschack, D.M. (1964), Effects of pressure and fluidpaturation on the attenuation of elastic waves in sands, J.Petr.Tech., 189–198.
Gupta, I.N., Burnetti, A., McElfresh, T.W., von Seggern, D.H., and Wagner, R.A. (1983), Lateral variations in attenuation of ground motion in the eastern United States based on propagation of Lg.NUREG/CR-3555, U.S. Nuclear Regulatory Commission, Washington, D.C.
Hermann, R.B. (1980), Q estimates using the coda of local earthquakes, Bull. Seism. Soc. Am., 70, 447–468.
Johnston, D.H., and Toksöz, M.N. (1980), Ultrasonic P and S wave attenuation in dry and saturated rocks under pressure, J.Geophys. Res., 85, 925–936.
Klima, K., Vanek, J., and Pros, Z. (1964), The attenuation of longitudinal waves in diabase and greywacke under pressure up to 4 kilobars, Studia Geoph. et Geod., 8, 247–254.
Knopoff, L. (1964), Q, Rev. Geophys., 2, 625–660.
Kopnichev, Y.F. (1977), The role of multiple scattering in the formation of a seismogram tail, Izv. Acad. Sci., USSR, Phys. Solid Earth, 13, 394–398.
Mason, W.P., Beshers, D.N., and kuo, J.T.,(1970),Internal friction in Westerly granite: Relation to dislocation theory, J.Appl. Phys., 41, 5206–5209.
Nur, A., and Winkler, K. (1980), The role of friction and fluid flow in wave attenuation in rocks (abst.), Geophysics, 45, 591–592.
O’Doherty, R.F., and Anstey, N.A.,(1971),Reflections on amplitudes, Geophys. Prospect., 19, 430–458.
Pandit, B.I., and Savage, J.C. (1973), An experimental test of Lomnitz’s theory of internal friction in rocks, J.Geophys. Res., 78, 6097–6099.
Peselnick, L., and Outerbridge, W.F. (1961), Internal friction in shear and shear modulus of Solenhofen limestone over a frequency range of 107 cycles per second, J.Geophys. Res., 66, 581–588.
Plona, T.J., Observation of a second bulk compressional wave in a porous medium at ultrasonic frequencies, Appl. Phys. Lett., 36, 256–261.
Plona, T.J., and Johnson, D.L. (1980), Experimental study of the two bulk compressional modes in water saturated porous structures,Ultrasonic Symposium, 864–872.
Pulli, J. (1984), Attenuation of coda waves in New England, Bull. Seism. Soc. Am., 74, 1149–1166.
Rautian, T.G., and Khalturin, V.I. (1978), The use of the coda for the determination of the earthquake source spectrum, Bull. Seism. Soc. Am., 1809–1827.
Richards, P.G., and Menke, W. (1983), The apparent attenuation of a scattering medium, Bull. Seism. Soc. Am. 73, 1005–1021.
Roecker, S.W., Tucker, B., King, J., and Hatzfled, D. (1982), Estimates of Q in central Asia as a function of frequency and depth using the coda of locally recorded earthquakes, Bull. Seism. Soc. Am., 72, 129–149.
Schmitt, D.P. (1985), Simulation numérique de diagraphies acoustiques. Propagation d’ondes dans des formations cylindriques axisymétriques radialement stratifiées incluant des milieux élastiques et/ou poreux saturés. Ph.D. thesis. Grenoble Univ.
Singh, S. (1985), Lg and coda wave studies of Eastern Canada, Ph.D. thesis Saint Louis University, Missouri.
Singh, S., and Hermann,R.B. (1983), Regionalization of crustal coda Q in the continental United States, J.Geophys. Res., 88, 527–538.
Spencer, J.W., Jr. (1981), Stress relaxations at low frequencies in fluid saturated rocks: attenuation and modulus dispersion. J.Geophys. Res., 86, 1803–1812.
Tittmann, B.R., Housley, R.M., Alers, G.A., and Cirlin, E.H. (1974), Internal friction in rocks and its relationship to volatiles on the moon, in Lunar Science Conf., 5th Proc., Geochim. et Cosmochim. Acta, suppl.
v.3, 2913–2918.
Tittmann, B.R., Nadler, H., Clark, V.A., Ahlberg,L.A., and Spencer,T.W. (1981), Frequency dependence of seismic dissipation in saturated rocks, Geophys. Res. Lett., 8, 36–38.
Toksöz, M.N., Johnston, D.H., and Timur,A. (1979), Attenuation of seismic waves in dry and saturated rocks. I.Laboratory measurements, Geophysics, 44, 681–690.
Toksöz, M.N., and Johnston, D.H. (1981), Seismic wave attenuation. Editors. Geophysics reprint series No.2. Society of Exploration Geophysicist.
Walfish, J.B. (1966), Seismic wave attenuation in rock due to fracture, J.Geophys. Res., 17, 2591–2599.
Winkler, K., and Nur, A. (1979), Pore fluids and seismic attenuation in rocks, Geophys. Res. Lett., 6, 1–4.
Wu, R.S. (1984), Multiple scattering and energy transfer of seismic waves and the application:òf the theory to Hindu Kush region, in “Seismic wave scattering and the small scall inhomogeneities in the lithosphere”, Chapter 4, Ph.D.thesis, Mass. Inst.Tech., Cambridge, M.A.
Wu, R.S., Multiple scattering and energy transfer of seismic waves. Separation of scattering effect from intrinsic attenuation. I.Theoretical modelling., Geophys. J. R.Astr. Soc., 82, 57–80.
Wu, R.S., and Aki.K. (1985), Multiple scattering and energy transfer of seismic waves. Separation of scattering effect from intrinsic attenuation. I I. Application of the theory to Hindu Kush region, submitted to J.Geophys. Res..
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 1987 Springer Science+Business Media Dordrecht
About this chapter
Cite this chapter
Toksöz, M.N., Wu, R.S., Schmitt, D.P. (1987). Physical Mechanisms Contributing to Seismic Attenuation in the Crust. In: Erdik, M.Ö., Toksöz, M.N. (eds) Strong Ground Motion Seismology. NATO ASI Series, vol 204. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-3095-2_9
Download citation
DOI: https://doi.org/10.1007/978-94-017-3095-2_9
Publisher Name: Springer, Dordrecht
Print ISBN: 978-90-481-8440-8
Online ISBN: 978-94-017-3095-2
eBook Packages: Springer Book Archive