Short-and long-term processes at or close to the subduction plate interface (eg, mineral
transformations, fluid release, seismicity and more generally deformation) might be more …

Subduction zones produce the largest earthquakes. Over the past two decades, space
geodesy has revolutionized our view of crustal deformation between consecutive …

The range of fault slip behaviors near the trench at subduction plate boundaries is critical to
know, as this is where the world's largest, most damaging tsunamis are generated. Our …

Among the wide range of thermal, petrologic, hydrological, and structural factors that
potentially affect subduction earthquakes, the roughness of the subducting seafloor is …

Subduction zone megathrust faults host Earth's largest earthquakes, along with multitudes of
smaller events that contribute to plate convergence. An understanding of the faulting …

Because of a combination of new observational tools and a flurry of large megathrust
earthquakes, tremendous progress has been made in recent years towards understanding …

Subduction faults, called megathrusts, can generate large and hazardous earthquakes. The
mode of slip and seismicity of a megathrust is controlled by the structural complexity of the …

Slow earthquakes are episodic slow fault slips. They form a fundamental component of
interplate deformation processes, along with fast, regular earthquakes. Recent …

Subduction of rough seafloor and seamounts is thought to impact a broad range of
geodynamic processes, including megathrust slip behaviour, forearc fluid flow and long-term …

We document a sequence of simultaneous short‐term and long‐term slow slip events
(SSEs) at the Hikurangi subduction zone during the 2010/2011 period. The sequence of …