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- W2095655707 abstract "To construct additional branches of the travel-time curve of PKP waves the residuals of travel times reported in the Bulletins were used. A part of GH branch has been obtained for epicentral distances Δ>145°. The results obtained separately by using the data for shallow and deep earthquakes are in good agreement. The mean slope of this branch was found to be similar to that obtained by ADAMS and RANDALL, but the value of the slope near the end of the branch is in better agreement with that proposed by Bolt. By using the data for deep shocks a part of the trevel-time curve was obtained corresponding to the forerunners for distances Δ<145°. This branch of the travel-time curve was found to be shifted down with respect to the branch GH. Therefore this branch cannot be interpreted as a continuation of GH." @default.
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- W2095655707 date "1968-01-01" @default.
- W2095655707 modified "2023-10-02" @default.
- W2095655707 title "Some data on seismic waves through the Earth's core" @default.
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- W2095655707 doi "https://doi.org/10.4294/jpe1952.16.37" @default.
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