Recurring slow slip along near-trench megathrust faults occurs at many subduction zones,
but for unknown reasons, this process is not universal. Fluid overpressures are implicated in …

In subduction zones, fluids are often invoked to explain slip processes on the megathrust,
from great earthquakes to slow-slip events and tectonic tremors. However, it is unclear how …

Nearly 3,500 methane bubble streams, clustered into more than 1,300 methane emission
sites, have been identified along the US Cascadia margin, derived both from archived …

Exploring the structure of convergent margins is key to understanding megathrust slip
behavior and tsunami generation. We present new wide‐angle and marine multichannel …

We study stress, pressure, and rock properties in evolving accretionary wedges using
analytical formulations and geomechanical models. The evolution of the stress state from …

Subducted sediment plays a key role in modulating pore pressure and seismic behavior at
subduction zones. We investigated the seismic character of incoming sediments to test how …

The Java‐Lesser Sunda margin, which features multi‐scale subducting oceanic basement
relief, is classified as neutral (Lombok and Sumbawa) to erosional (Central Java to Bali) in …

In subduction zones, along‐strike and downdip variations in megathrust slip behavior are
linked to changes in properties of the subducting and overriding plates. Although marine …

On 19 October 2020, an M w 7.6 earthquake occurred within the Shumagin Islands, Alaska,
which is the largest strike‐slip earthquake occurred in the shallow subducted plates with …

Along the Hikurangi subduction margin, on the east coast of New Zealand's North Island, the
interplate coupling changes from locked in the south to weakly coupled in the north. New …