Abstract
A method to tomographically image the spatial variation of group velocity across a region of geologic interest has been developed. The tomographic algorithm used represents a development of the Simultaneous Iterative Reconstruction Techniques (SIRT). It includes a ray tracing capability. The principal advantage of this method over previously described methods is that it permits the dispersion function to vary continuously over the region. Computer simulations and the results from some field tests in Texas demonstrate the utility of this method.
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References
Abo-Zena, A., 1979, Dispersion function computation for unlimited frequency values: Geoph. J., v. 58, p91.
Dines, K.A., and Lytle, R.J., 1979, Computerized geophysical tomography: Proc. IEEE, v. 67, p1065.
Dziewonski, A., Bloch, S., and Landisman, M., 1 9 6 9, A technique for the analysis of transient seismic signals: Bull. Seis. Soc. Am., v.59, p427.
Ewing, M., and Press, F., 1950, Crustal structure and surface wave dispersion: Bull. Seis. Soc. Am., v. 40, p271.
Gilbert, P., 1972, Iterative methods for the three-dimensional reconstruction of an object from projections: J. Theor. Biol., v. 36, p105.
Gordon, R., Bender, R., and Herman, G.T., 1 970, Algebraic Reconstruction Techniques (ART) for three-dimensional electron microscopy and x-ray photography: J. Theor. Biol, v.29, p47 1.
Lytle, R.J., and Dines, K.A., 1980, Iterative ray tracing between boreholes for underground image reconstruction: IEEE Trans. Geosci. and Remote Sensing, GE-18
Mason, I.M., 1981, Algebraic reconstruction of a two-dimensional velocity inhomogeneity in the High Hazles seam of Thoresby colliery: Geophysics, v.46
Santo, T.A., 1960, Rayliegh wave dispersion across the oceanic basin around Japan, 2: Bull. Earthquake Res. Inst. Tokyo Univ., v. 38, p385.
Santo, T.A., 1961, Division of the south-western Pacific area into several regions in which Rayliegh waves have the same dispersion charadters: Bull. Earthquake Res. Inst. Tokyo Univ., v. 39, p603.
Santo, T.A., 1 965, Lateral variation of Rayliegh wave dispersion character, 2, Eurasia: Pure Appl. Geophys., v.62, p 67
Santo, T.A.,1 966, Lateral variation of Rayliegh wave dispersion character, 3, Atlantic Ocean, Africa, and Indian Ocean: Pure Appl. Geophys., v.63, p40.
Sheridan, R., 1972, Crustal structure of the Bahama platform from Rayliegh wave dispersion: JGR, v. 77, p2139.
Shurbet, D.H., 1960, The effect of the Gulf of Mexico on Rayliegh wave dispersion: JGR, v. 65, p40.
Shurbet, D.H., 1961. Determination of sedimentary thickness in the Mexican geosynclme by Rayliegh wave dispersion: JGR, v. 66, p899.
Tarr, A.C., 1 969, Rayliegh wave dispersion in the North Atlantic Ocean, Caribbean Sea, and Gulf of Mexico: JGR, v.74, p159.
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© 1984 Plenum Press, New York
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Wattrus, N.J. (1984). Seismic Tomography Applied to Surface Wave Analysis. In: Kaveh, M., Mueller, R.K., Greenleaf, J.F. (eds) Acoustical Imaging. Acoustical Imaging, vol 13. Springer, Boston, MA. https://doi.org/10.1007/978-1-4613-2779-0_45
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DOI: https://doi.org/10.1007/978-1-4613-2779-0_45
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