The discipline of seismology is based on observations of ground motion that are inherently
undersampled in space and time. Our basic understanding of earthquake processes and our …

The record of seismic, hydroacoustic, and infrasonic waves is essential to detect, identify,
and localize sources of both natural and anthropogenic origin. To guarantee traceability and …

Train traffic has recently been realized as a potential seismic source for imaging and
monitoring shallow subsurface structures. High-speed trains usually move on viaducts and …

Microseismic noise has been used for seismic velocity monitoring. However, such signals
are dominated by low‐frequency surface waves that are not ideal for detecting changes …

We utilize train tremors as P‐wave seismic sources to investigate velocity‐strain sensitivity
near the San Jacinto Fault Zone. A dense nodal array deployed at the Piñon Flat …

Train traffic has been realized as a powerful seismic source for imaging and monitoring the
shallow subsurface. High-speed trains running on viaducts generate seismic waves through …

Abstract The Alto Tiberina Fault system, located in the Northern Apennines (Italy), consists of
a low angle normal fault (LANF) which radiates micro‐seismicity that can be explained by …

Abstract The Imperial Valley is a seismically active basin occupying the southern end of the
Salton trough, an area of rapid extension, high heat flow, and abundant geothermal …

Dense seismic array monitoring combined with advanced processing can help retrieve and
locate a variety of seismic sources with unprecedented resolution and spatial coverage. We …

Body wave extraction from oceanic secondary microseismic sources with seismic
interferometry provides alternative information to better constrain the Earth's structure …