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 …

It is generally accepted that tectonic earthquakes may trigger volcanic activity, although the
underlying mechanisms are poorly constrained. Here, we review current knowledge, and …

Modern geodetic and seismologic observations describe the behavior of fault slip over a
vast range of spatial and temporal scales. Slip at sub-seismogenic speeds is evident from …

Tectonic faults fail in a spectrum of modes, ranging from earthquakes to slow slip events.
The physics of fast earthquakes are well described by stick–slip friction and elastodynamic …

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 …

Abstract Multiple (> 20) crustal faults ruptured to the ground surface and seafloor in the 14
November 2016 M w 7.8 Kaikōura earthquake, and many have been documented in detail …

Reusing waste materials to create energy harvester will not just reduce the environmental
pollution, but also generate renewable electricity by scavenging environmental energy to …

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 …

Abstract The Hikurangi subduction margin, New Zealand, has not produced large
subduction earthquakes within the short written historic period (~ 180 years) and the …

Abstract The 2016 MW7. 8 Kaikōura earthquake ruptured a complex sequence of strike‐slip
and reverse faults in New Zealand's northeastern South Island. In the months following the …