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Phase statistics of seismic coda waves.
D Anache-Ménier1, B A van Tiggelen, L Margerin
1Laboratoire de Physique et de Modélisation des Milieux Condensés, Université Joseph Fourier/CNRS, BP 166, 38042 Grenoble, France.
Physical Review Letters
|August 8, 2009
Summary
Seismic coda phase fluctuations follow universal power-law decays, matching Gaussian statistics. This analysis helps estimate the mean free path of Rayleigh waves, crucial for understanding seismic wave propagation.
Area of Science:
- Seismology
- Wave Propagation Physics
Background:
- Seismic coda waves contain valuable information about Earth's subsurface structure.
- Understanding seismic wave scattering is key to interpreting earthquake recordings.
Purpose of the Study:
- To analyze phase fluctuation statistics in earthquake seismic coda.
- To compare observed distributions with theoretical statistical models.
- To estimate the mean free path of seismic waves.
Main Methods:
- Deployment of a temporary seismic experiment at Pinyon Flats Observatory, California.
- Statistical analysis of seismic coda phase fluctuations.
- Measurement of the phase derivative correlation function.
Main Results:
- Observed distributions of spatial phase derivatives exhibit universal power-law decays.
- Exponents of these power laws accurately agree with circular Gaussian statistics.
- The correlation function provided an estimate for the mean free path of Rayleigh waves.
Conclusions:
- Seismic coda phase fluctuations are well-described by universal statistical laws.
- Circular Gaussian statistics accurately model these phenomena.
- The study provides a method for estimating the mean free path of Rayleigh waves from coda analysis.
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