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 …

We present a suite of 15 palaeogeographic maps illustrating the geological evolution of the
entirety of Zealandia, from mid-Cretaceous to present, highlighting major tectonic phases …

Asgardarchaeota have been proposed as the closest living relatives to eukaryotes, and a
total of 72 metagenome-assembled genomes (MAGs) representing six primary lineages in …

In subduction zones, seismic slip at shallow crustal depths can lead to the generation of
tsunamis. Large slip displacements during tsunamogenic earthquakes are attributed to the …

The role of subducting topography on the mode of fault slip—particularly whether it hinders
or facilitates large megathrust earthquakes—remains a controversial topic in subduction …

Slow slip events (SSEs) have been identified at subduction zones globally as an important
link in the continuum between elastodynamic ruptures and stable creep. The northern …

Geophysical observations show spatial and temporal variations in fault slip style on shallow
subduction thrust faults, but geological signatures and underlying deformation processes …

New biostratigraphically constrained chronologies have been developed to help elucidate
the sedimentary and tectonic history of Quaternary sequences on the Hikurangi margin of …

Laboratory measurements can determine the potential for geologic materials to generate
unstable (seismic) slip, but a direct relation between sliding behavior in the laboratory and …

Many described subduction complexes (or mélanges) exhumed from seismogenic depths
comprise thick, turbidite‐dominated sequences with deformed zones containing clasts or …