The ambient seismic wave field, also known as ambient noise, is excited by oceanic gravity
waves primarily. This can be categorized as seismic hum (1–20 mHz), primary microseisms …

Ambient noise tomography has proven to be effective in resolving shallow earth structure.
We applied ambient noise tomography on a dense seismic array in Long Beach, California …

The cross correlation of ambient signal allows seismologists to collect data even in the
absence of seismic events.“Seismic interferometry” shows that the cross correlation of …

We retrieve P diving waves by applying seismic interferometry to ambient‐noise records
observed at Long Beach, California, and invert travel times of these waves to estimate 3‐DP …

Significant left-lateral movement along the Ailao Shan-Red River fault accommodated a
substantial amount of the late Eocene to early Miocene India-Asia convergence. However …

We utilize an array method called the frequency‐Bessel transformation method to extract the
multimodal dispersion curves of Rayleigh waves from ambient seismic noise data recorded …

We proposed a new passive seismic method (PSM) based on seismic interferometry and
multichannel analysis of surface waves (MASW) to meet the demand for increasing …

We present here a global analysis showing that wave paths probing the deepest part of the
Earth can be obtained from ambient noise records. Correlations of seismic noise recorded at …

We present a new 3-D seismic model of the western United States crust derived from a joint
inversion of Rayleigh-wave phase velocity and ellipticity measurements using periods from …

Seismic body waves that sample Earth's core are indispensable for studying the most
remote regions of the planet. Traditional core phase studies rely on well‐defined earthquake …