The structure of the earth has been extensively studied using seismic waves generated by
natural earthquakes and man-made sources. In classical seismology, the earth is …

Equipartition is a first principle in wave transport, based on the tendency of multiple
scattering to homogenize phase space. We report observations of this principle for seismic …

We first present a summary of recent results on coda interpretation. We emphasize the
observation of the stabilization of P to S energy ratio indicating the modal equipartition of the …

We demonstrate the existence of long‐range field correlations in the seismic coda of
regional records in Alaska. The cross correlations between the different components of coda …

Since its deployment at the surface of Mars, the Seismic Experiment for Interior Structure
(SEIS) instrument of the InSight mission has detected hundreds of small‐magnitude seismic …

Multiple-scattered waves usually are not useful for creating deterministic images of the
interior of elastic media. However, in many applications, one is not so much interested in …

Coda-wave interferometry is a technique which exploits tiny waveform changes in the coda
to detect temporal variations of seismic properties in evolving media. Observed waveform …

The reconstruction of seismic Green's functions from correlations of ambient seismic noise
has recently developed as a promising approach for exploring the earth's interiors without …

At high frequencies (∼ 1 Hz), much of the seismic energy arriving at teleseismic distances is
not found in the main phases (eg P, PP, S, etc.) but is contained in the extended coda that …

The coda quality factor of short‐period S waves (Q c) excited by local earthquakes in the
Pyrenees has been measured as a function of the length of the coda window (LW) for …