Continuously operating global positioning system sites in the North Island of New Zealand
have revealed a diverse range of slow motion earthquakes on the Hikurangi subduction …

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

Slow slip events (SSEs) accommodate a significant proportion of tectonic plate motion at
subduction zones, yet little is known about the faults that actually host them. The shallow …

Slow slip events are part of a spectrum of aseismic processes that relieve tectonic stress on
faults. Their spatial distribution in subduction zones has been linked to perturbations in fluid …

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 …

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 …

The recognition of slow earthquakes in geodetic and seismological data has transformed the
understanding of how plate motions are accommodated at major plate boundaries. Slow …

We use a prestack depth migration reflection image and magnetic anomaly data across the
northern Hikurangi subduction zone, New Zealand, to constrain plate boundary structure …

Fluid migration and pore fluid pressure have been implicated in generating the transitional
fault zone properties thought to be important for slow slip events (SSEs) in subduction …

The Guerrero seismic gap is presumed to be a major source of seismic and tsunami hazard
along the Mexican subduction zone. Until recently, there were limited observations at the …