Abstract
Digitally-recorded waveforms from foreshocks and aftershocks of the October 18, 1981, Eniwa, Hokkaido, earthquake (M=4.0)are compared. The foreshock activity exhibits the pattern similar to a main shock-aftershock sequence. Four consecutive foreshocks (M= −0.1 to 1.3) that occurred during one hour and a half before the main shock have strongly similar waveforms. An average value of peak cross-correlations for pairs of foreshock seismograms is 0.86. The bandpass-filtered waveforms are well correlated at frequencies up to at least 20 Hz. This implies similar source mechanisms and tight clustering of hypocenters within a radius of no more than 1/4 wavelength, i.e., 70 m or less. Aftershock waveforms are variable from one event to the next, although at least four groups of similar events are found during the aftershock period. The present exercise provides one approach to the identification of a foreshock sequence on the basis of remarkably similar waveforms.
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© 1985 Springer Science+Business Media Dordrecht
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Motoya, Y., Abe, K. (1985). Waveform Similarity among Foreshocks and Aftershocks of the October 18, 1981, Eniwa, Hokkaido, Earthquake. In: Kisslinger, C., Rikitake, T. (eds) Practical Approaches to Earthquake Prediction and Warning. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-2738-9_24
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DOI: https://doi.org/10.1007/978-94-017-2738-9_24
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