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- W2089969767 abstract "SummaryAn examination of six near earthquakes in Western and Central Europe indicates that the velocity of P in this region is somewhat higher than in Southern Europe and Japan, the difference in dt/dΔ being about os.5/1°. The agreement found in a previous comparison is attributed to a possibility that P in the Tauern earthquake was read late owing to weakness. Apart from the Tauern earthquake the earthquakes used in previous discussions are consistent with the existence of the difference. The results are consistent with the observations of the Burton-on-Trent explosion provided that the foci were shallow, probably within the sedimentary layer. The direct examination of Pg and Sg at short distances leads to a suggestion of differences of focal depth, but this is contradicted by the comparison of P with Pg and of S with Sg. The chief anomaly outstanding is that the comparison of P with Pg suggests an increase in the allowance for the upper layers for a surface focus, that of S with Sg a decrease; the residuals of S and Sg show discrepancies at several points from the hypothesis that the errors are purely random, but their distribution does not suggest any explanation." @default.
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- W2089969767 date "1947-05-01" @default.
- W2089969767 modified "2023-09-27" @default.
- W2089969767 title "SEISMIC WAVES IN WESTERN AND CENTRAL EUROPE" @default.
- W2089969767 doi "https://doi.org/10.1111/j.1365-246x.1947.tb00346.x" @default.
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