Synonymer & Information om | Engelska ordet P-WAVE

Exempel på hur man kan använda P-WAVE i en mening

• The result is a lengthening of the R-R intervals as each subsequent P-wave reaches an increasingly refractory AV node until the impulse fails to conduct, which ultimately results in a blocked QRS complex.
• P-wave arrivals from LFEs have amplitudes so small that they are often difficult to detect, so when the JMA first distinguished the unique class of earthquake it was primarily by the detection of S-wave arrivals which were emergent.
• The equations are important in geophysics because they relate the amplitude of P-wave, incident upon a plane interface, and the amplitude of reflected and refracted P- and S-waves to the angle of incidence.
• Estimates suggest an approximately 40 km thick layer of moderately serpentinized mantle would be sufficient to explain the observed seismic P-wave attenuations associated to events occurring at depths of around 5–35 km below the Wadati–Benioff zone.
• The P-wave and S-wave velocities (Vp and Vs) of pyrolite along the 1600 K adiabatic geotherm are shown in Fig.
• A teleseismic P-wave will generate P-to-S conversions at boundaries, such as the Moho (crust-mantle boundary), beneath the seismograph.
• However, evidence of propagation at velocities between S-wave and compressional wave (P-wave) values have been reported for several earthquakesArchuleta,R.
• When a P-wave is detected from two (or more) of the 4,235 seismometers installed throughout Japan, the JMA analyzes and predicts the approximate location of the earthquake's epicenter.
• SV-wave microseisms are observed to be excited in the same place as P-wave microseisms, and can be explainable in the same theory of P-wave microseisms.
• Using newly implemented telemetric seismographic stations, they were able to record both P-wave and S-wave arrivals from earthquakes up to 260 km beneath the volcanic area.

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