Abstract
The amplitude ratio of the maximum motion before Sn (Pmax) to the maximum after Sn (Lg) is a good discriminant between earthquakes and explosions at regional distances. Experimental data shows that the ratio is not seriously affected by site or source geology or by event depth. However propagation effects can be severe, especially from the USSR to the South, and can lead to the requirement for regionalization. The amplitude-distance relation for Pmax and Lg is A ~ r−3 in the Western United States (WUS), and r−2.5 and r−2.0 for Pmax and Lg respectively in the EUS and within the USSR. The radial to transverse ratio for Lg does not appear to be a discriminant, being controlled by the local geology. Evidence is presented that there are no useful spectral discriminants in the 1 to 10 Hz band. It appears that spectra of Lg are contaminated by compressional wave coda which can lead to an overestimate of the high frequency energy in the direct Lg wave.
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Blandford, R.R. (1981). Seismic Discrimination Problems at Regional Distances. In: Husebye, E.S., Mykkeltveit, S. (eds) Identification of Seismic Sources — Earthquake or Underground Explosion. NATO Advanced Study Institutes Series, vol 74. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-8531-5_38
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DOI: https://doi.org/10.1007/978-94-009-8531-5_38
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