The discipline of seismology is based on observations of ground motion that are inherently
undersampled in space and time. Our basic understanding of earthquake processes and our …

Abstract The complex 2016 MW 7.8 Kaikōura earthquake ruptured> 20 faults and caused
highly variable uplift and subsidence of an~ 110 km stretch of coastline. The earthquake …

Using a new integrated earthquake catalog for Aotearoa New Zealand (described in a
companion article), we estimate the magnitude–frequency distributions (MFDs) of …

ABSTRACT The Kaikōura Earthquake uplifted Kaikōura Peninsula by≤∼ 1 m. Uplift in 2016
mainly resulted from slip on an offshore thrust fault (OSTF), modelled to splay from the plate …

Relative relocation techniques are widely used to improve the resolution of earthquake
hypocenter positions. Here, we present GrowClust3D. jl—an open‐source software package …

We investigate spatiotemporal changes of intermediate‐depth earthquakes in the double
seismic zone beneath Central and Northeastern Japan before and after the 2011 magnitude …

In this paper, a template matching and location method, which has been rapidly adopted in
microseismic research in recent years, is applied to laboratory acoustic emission (AE) …

Paleoseismic evidence from the late‐interseismic Alpine Fault suggests key section
boundaries conditionally inhibit rupture. We utilize a year of data from a two‐part …

Abstract The 2016 moment magnitude 7.8 Kaikoura, New Zealand, earthquake occurred at
the southern end of the Hikurangi subduction zone where the upper plate above the shallow …

ABSTRACT The Kaikōura Earthquake ruptured a complex network of at least 20 faults in the
northeastern South Island, with variable geometries, slip and slip rates. Ground shaking and …