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Bulletin of the Seismological Society of America; February 2007; v. 97; no. 1B; p. 198-207; DOI: 10.1785/0120060096
© 2007 Seismological Society of America
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Imaging the Upper Crust of the Korean Peninsula by Surface-Wave Tomography

K. H. Cho1, R. B. Herrmann2, C. J. Ammon3 and K. Lee1

1 School of Earth and Environmental Sciences
Seoul National University
Seoul 151-742, South Korea
 (K.H.C, K.L)
2 Department of Earth and Atmospheric Sciences
Saint Louis University, 203 O’Neil Hall
3642 Lindell Boulevard
St. Louis, Missouri 63108
 (R.B.H.)
3 Department of Geosciences
Penn State University, Deike Bldg.
University Park, Pennsylvania 16802
 (C.J.A)

Cross correlation of seismic-background motions (Campillo and Paul, 2003; Shapiro et al., 2005) is applied to observations from the Korean Meteorological Administration seismic network to estimate the short-period Rayleigh and Love wave dispersion characteristics of the region. Standard processing procedures are applied to the cross correlation, except that signal whitening is used in place of one-bit sampling to equalize power in signals from different times. Multiple-filter analysis is used to extract the group velocities from the estimated Green’s functions, which are then used to image the spatially varying dispersion at periods between 0.5 and 20 sec. The tomographic inversion technique used inverts all periods simultaneously to provide a smooth dispersion curve as a function of period in addition to the usual smooth spatial image for a given period. The Gyeongsang Basin in the southeastern part of the peninsula is clearly resolved with lower group velocities.




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