= Coda wave interferometry
{wiki=Coda_wave_interferometry}
Coda wave interferometry is a seismic analysis technique used to investigate the properties of the Earth's interior and to monitor changes in subsurface structures. It leverages the analysis of coda waves, which are the later arriving waves in a seismic signal that follow the direct waves (such as P and S waves) after an earthquake or artificial seismic event. Coda waves are formed by multiple scattering of seismic waves within and around the seismic source region.
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