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- W2113704003 abstract "Spectrum analyses have been made of T phases that have traveled from earthquakes and explosions in the Atlantic Ocean to a recording point over completely oceanic paths and over paths having a very short continental segment at the source end. A great deal of the variability in T-phase velocity previously reported in the literature is due to uncertainty of correction for the land portion of the path. However, even with a completely oceanic path there are variations in the apparent velocity of T for earthquakes although not for explosions. These variations are due primarily to the T-phase arrival being dispersive. Only the higher frequencies (50 to 150 cps) travel with the velocity of sound in water. The transformed energy received at a seismograph on land usually shows only a small part of the spectrum, so that the travel time will depend on instrumental characteristics and sensitivity as well as on the travel path. The sound spectrograph records are symmetrical in time about the peak signal. The earliest T arrivals are abrupt when a proper broad-band instrument is used. They arrive with a velocity as high as 1.65 km/sec, corresponding to possible transmission through the sediments. The large central spike containing the high-frequency arrivals has the velocity of sound in water in the Sofar channel (1.49±0.005 km/sec in the Atlantic); the later arrivals are caused by later modes and reverberation." @default.
- W2113704003 created "2016-06-24" @default.
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- W2113704003 date "1962-07-01" @default.
- W2113704003 modified "2023-09-27" @default.
- W2113704003 title "Evidence of dispersion in earthquakeTphases" @default.
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- W2113704003 doi "https://doi.org/10.1029/jz067i007p02823" @default.
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