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 …

Abstract The 2016 M7. 8 Kaikōura earthquake is one of the most complex earthquakes in
recorded history, with significant rupture of at least 21 crustal faults. Using a matched‐filter …

Earthquake swarms, which are anomalous increases in the seismicity rate without a
distinguishable mainshock, often accompany transient aseismic processes, such as fluid …

Slow-slip events at global subduction zones relieve tectonic stress over days to years.
Through slow-slip cycles, high fluid pressures observed at the top of subducting plates are …

Assessing the stability state of fault interfaces is a task of primary interest not only for seismic
hazards, but also for understanding how the earthquake machine works. Nowadays it is well …

We report the first catalog of low‐frequency earthquakes in the Hikurangi subduction zone,
located beneath the Kaimanawa Range of the North Island at 50 km depth, downdip of …

We develop a methodology to compile an objective tremor catalog by utilizing distinctive
event features that differentiate tectonic tremors from non‐tremor events, and combining the …

Slow slip events (SSEs) are geophysical phenomena primarily occurring in subduction
zones. These events are often associated with seismic activity and can be detected by …

The Manawatu region experiences deep tremor and long‐term slow slip events (SSEs);
however, tremor is adjacent to, and not co‐located with, long‐term SSEs. Observations of …