Quantitative Seismology¶
Aki, K., & Richards, P. G. (2002). Quantitative Seismology. University Science Books.
Cited by¶
3 citations across 3 artifacts.
Each citation links to the sentence it supports in the citing article.
Primes¶
- Dispersion
- In acoustics and seismology, wave packets composed of multiple frequencies spread in dispersive media because phase velocity depends on frequency, and seismic surface waves are interpreted by inverting the dispersion relation to recover earth structure.
This sourceSurface-wave dispersion (frequency-dependent phase velocity) inverted to recover Earth structure.
- In acoustics and seismology, wave packets composed of multiple frequencies spread in dispersive media because phase velocity depends on frequency, and seismic surface waves are interpreted by inverting the dispersion relation to recover earth structure.
Domain-specific¶
- Anelastic attenuation factor
- Wave Packet
- Quantum mechanics — a free particle's wavefunction is a Gaussian wave packet whose group velocity equals the classical velocity p/m and whose spreading is the time-evolution of position uncertainty. Ultrafast optics and telecom — femtosecond laser pulses as optical wave packets, with chirp, group-velocity dispersion, and fibre pulse-compression all computed from the fibre's dispersion relation. Seismology — a ground-motion burst as a seismic packet whose frequency-dependent group velocity reconstructs the layered structure of crust and mantle
This sourceGraduate text treating surface-wave dispersion in vertically layered Earth models, including its measurement from seismograms and the sensitivity of phase velocity to structure.
Supported in partVerified against the source
- Quantum mechanics — a free particle's wavefunction is a Gaussian wave packet whose group velocity equals the classical velocity p/m and whose spreading is the time-evolution of position uncertainty. Ultrafast optics and telecom — femtosecond laser pulses as optical wave packets, with chirp, group-velocity dispersion, and fibre pulse-compression all computed from the fibre's dispersion relation. Seismology — a ground-motion burst as a seismic packet whose frequency-dependent group velocity reconstructs the layered structure of crust and mantle
Verification¶
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