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SEISMIC DATA ANALYSIS CENTER TELEDYNE GEOTECH, P.O. BOX 334, ALEXANDRIA, VIRGINIA 22314
Abstract
It is shown that principal component analysis (eigenvector-eigenvalue decomposition of array spectral matrices) can be used for the approximate separation of superposed plane-wave signals only if at least one of the following conditions is satisfied:
Application of the method for such cases is demonstrated on composited long-period seismograms using recordings from the D ring and center element of ASA.
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