Physics
Scientific paper
Mar 1992
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992georl..19..557f&link_type=abstract
Geophysical Research Letters (ISSN 0094-8276), vol. 19, March 20, 1992, p. 557-560. Research supported by DARPA, USAF, and W.M.
Physics
Coherence Coefficient, Lithosphere, Phased Arrays, Seismology, Earth Crust, Earth Mantle, Root-Mean-Square Errors, Wave Scattering
Scientific paper
The transverse coherence function (TCF) of arrival time is investigated with data from two arrays to evaluate the TCFs for spatial separations of 100 m up to 80 km. Data from arrays of varying apertures are combined by studying rms fluctuations and rms tilts on each array, and the results are compared to those of synthetic fluctuation fields with specific statistical properties. Array size is found to have a significant effect on statistical observations of rms fluctuation and tilt as well as on coherence analysis, and the TCFs resulting from the technique are found to be compatible with the inhomogeneity model by Flatte et al. (1991).
Flatte Stanley M.
Xie Xiao-Bi
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