Abstract
Single-station three-component analysis is applied to seismic recordings in Norway from quarry blasts on the Kola peninsula. Even for P-waves, non-linear particle motions are observed, implying phase shifts between the horizontal and vertical components. Such instantaneous phase-lags provide direct and useful information on the arrival of different wave types, and this is illustrated. For P-waves, the most probable origin of these phase shifts is scattering and P-to-S conversion. Phase-lags are also observed for later phases. Using signal particle motion models which allow for phase shifts we have been successful in analysing several different phases (P, S and Lg) in these complex regional events. Such results contrast with various previous studies of this and similar data, in which three-component analysis was found to be relatively ineffective. We attribute this significant difference in results in part to sub-optimal processing parameters and/or three-component analysis methods in some of the earlier studies e.g. analysis based on visual inspection of particle motion figures (very difficult where phase-lags are involved) or on eigenvector analysis where the diagonal elements of the covariance matrix, and thus uncorrelated noise, have a large influence. Incorporating seismic wavefield physics leads to signal models which can be expressed primarily in terms of off-diagonal elements and such models are therefore inherently more robust.
The relative information content and thus cost-effectiveness of single-component arrays and three-component data are compared, and our results indicate that in many circumstances the three-component configuration is by far the most cost-effective.
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References
Hu G., Menke W. and Rögnvaldsson S.Th. (1993) A demonstration of the joint use of P-wave polarization and travel-time data in tomographic inversion: Crustal velocity structure near the South Iceland Lowland Network. Geophys. Res. Lett. 20 1407–1410.
Roberts R.G., Lindfors A., Christoffersson A., Bödvarsson R. and Rögnvaldsson S.Th. (1993) Three-component data as an aid to seismic event detection and association: A case study using data from the SIL (Iceland) network. Computers and Geosciences 19 123–134.
Kvaerna T, and Ringdal F. (1992) Integrated array and three-component processing using a seismic microarray. Bull. Seis. Soc. Am. 82 870–882.
Roberts R.G. and Christoffersson A. (1990) Decomposition of complex single-station three-component seismograms. Geophys. J. Int 103 57–74.
Jepsen D.C. and Kennett B.L.N. (1990) Three-component analysis of regional seismograms. Bull. Seis. Soc. Am. 80 2032–2052.
Magotra N., Ahmed N., Chael E. (1987) Seismic event detection and source location using single-station three-component data. Bull. Seis. Soc. Am. 77 958–971.
Jurkevics A. (1988) Polarization analysis of three-component array data. Bull. Seis. Soc. Am. 78 1725–1743.
Der Z.A., Baumgardt D.R. and Shumway R.H. (1993) The nature of particle motion in regional seismograms and its utilization for phase identification. Geophys. J. Int. 115 1012–1024.
Christoffersson A., Husebye E.S. and Ingate S. (1988) Wavefield decomposition using ML probabilities in single-site three-component records. Geophys. J. 93 197–213
Roberts R.G. and Christoffersson A. (1991) Seismic signal detection. A better mousetrap ? Bull. Seis. Soc. Am. 81 2511–2515.
Hestholm S.O., Husebye E.S. and Ruud B.O. (1994) Seismic wave propagation in complex crust-upper mantle media using 2-D finite difference synthetics. Geophys. J. Int. 118 643–670.
Ruud B.O. and Husebye E.H. (1992) A new three-component detector and automatic single-station bulletin production. Bull Seis. Soc. Am. 82 221–237
Ruud B.O., Lindholm C.D. and Husebye E.H. (1993) An exercise in automating seismic record analysis and network bulletin production. Bull. Seis. Soc. Am. 83 660–679.
Roberts R.G., Christoffersson A. and Cassidy F. (1989) Real time event detection, phase identification and source location estimation using single-station three-component seismic data. Geophys. J. Int. 97 471–480.
Stefansson R., Bödvarsson R., Slunga R., Einarsson P., Jakobsdottir J., Bungum H., Gregresen S., Havskov J., Hjelme J. and Korhonen H. (1993) The SIL project, background and perspectives for earthquake prediction in the South Iceland Seismic Zone. Bull Seis. Soc. Am. 83 696–716.
Taner M.T., Koehler F. and Sheriff R.E. (1979) Complex seismic trace analysis. Geophysics 44 1041–1063.
Park J., Vernon F.L. and Lindberg C.R. (1987) Frequency dependent polarization analysis of high frequency seismograms. J. Geophys. Res. 92 12664–12674.
Der Z. A., Shumway R.H. and Lees A.C. (1987) Multi-channel deconvolution of P waves at seismic arrays. Bull. Seis. Soc. Am. 77 195–211.
Lindfors A. and Roberts R.G. (1994) Array processing via phase regression.This volume.
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© 1996 Springer Science+Business Media Dordrecht
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Christoffersson, A., Roberts, R. (1996). Trinity or Verity ?. In: Husebye, E.S., Dainty, A.M. (eds) Monitoring a Comprehensive Test Ban Treaty. NATO ASI Series, vol 303. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-0419-7_32
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DOI: https://doi.org/10.1007/978-94-011-0419-7_32
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