Seismic interferometry from correlated noise sources
Daniella Ayala-Garcia, Andrew Curtis, Michal Branicki

TL;DR
This paper investigates the impact of correlated noise sources on seismic interferometry, revealing significant errors and proposing a new workflow to mitigate these effects, thereby enhancing subsurface imaging accuracy.
Contribution
It introduces a novel analytical approach and workflow to reduce errors caused by correlated noise sources in seismic interferometry, improving the reliability of Green's function estimates.
Findings
Correlated noise sources significantly perturb Green's function estimates.
Stacking reduces phase errors but does not fully eliminate issues caused by correlation.
The proposed workflow effectively mitigates errors from correlated ambient noise.
Abstract
It is a well-established principle that cross-correlating seismic observations at different receiver locations can yield estimates of band-limited inter-receiver Green's functions. This principle, known as seismic interferometry, is a powerful technique that can transform noise into signals which allow us to remotely image and interrogate subsurface Earth structures. In practice it is often necessary and even desirable to rely on noise already present in the environment. Theory that underpins many applications of ambient noise interferometry makes an assumption that the noise sources are uncorrelated in space and time. However, many real-world noise sources such as trains, highway traffic and ocean waves are inherently correlated both in space and time, in direct contradiction to the current theoretical foundations. Applying standard interferometric techniques to recordings from…
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