How an earthquake rupture propagates strongly influences the potentially destructive
ground shaking. Complex ruptures often involve slip along multiple faults, which masks …

Lithospheric seismic anisotropy illuminates mid‐ocean ridge dynamics and the thermal
evolution of oceanic plates. We utilize short‐period (5–7.5 s) ambient‐noise surface waves …

From 2011 to 2013, the CHINArray project led by the Institute of Geophysics, China
Earthquake Administration, made the first phase deployment of 350 broadband …

We present a new compilation and analysis of broad-band ocean bottom seismometer noise
properties from 15 yr of seismic deployments. We compile a comprehensive data set of …

We conduct a P‐wave receiver function analysis of the Bransfield Strait (West Antarctica) to
determine the lithospheric structure of this back‐arc basin, thanks to 31 temporary and …

Accurate marine sediment characteristics, for example, thickness and seismic velocity, are
important for constraining sedimentation rates with implications for climate variations and for …

Single-station and array ambient vibration techniques are widely used in onshore
environments, in particular to retrieve the subsurface structure and shear-wave velocity …

To establish a robust method of determining and correcting the misorientation of
seismometers with radial and tangential components of the teleseismic receiver function …

Megathrust earthquake behavior in subduction zones is controlled by a variety of factors
including the hydration state of the subducting slab. Increased hydration reduces the occur …

A significant amount of stress in the Cascadia subduction zone (CSZ) is released by different
forms of slow earthquakes including tremors, low‐frequency earthquakes, and very low …