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 …

We use cross-correlations of ambient seismic noise between pairs of 158 broadband and
short-period sensors to investigate velocity structure over the top 5–10 km of the crust in the …

We present a new technique for deriving detailed information on seismic velocities of the
subsurface material from continuous ambient noise recorded by spatially dense seismic …

We observe seasonal seismic wave speed changes (dv/v) in the San Jacinto fault area and
investigate several likely source mechanisms. Velocity variations are obtained from analysis …

We present tomographic images of crustal velocity structures in the complex Hot Springs
and Trifurcation areas of the San Jacinto Fault Zone (SJFZ) based on double-difference …

A self‐consistent regional‐scale seismic velocity model with resolution from seismogenic
depth to the surface is crucial for seismic hazard assessment. Though Southern California is …

We have analyzed the time-dependent properties of the ambient seismic wavefield between
0.1 and 8 Hz to detect, resolve, monitor, and image the deformation induced by the water …

SUMMARY Cross-correlations of 2–35 Hz ambient seismic noise recorded by three linear
arrays across the San Jacinto Fault Zone (SJFZ) in Southern California are used to derive …

Using seismic noise based monitoring techniques we find that seismic velocity variations
(dv/v) observed with the borehole array of the Taiwan Chelungpu-fault Drilling Project …

We image the subsurface below a dense seismic array straddling the Clark branch of the
San Jacinto fault zone in Southern California. The analysis is based on focal spots of surface …