Add to ORKGSlow 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 depth (<2 km) of well-documented SSEs at the Hikurangi subduction zone offshore New Zealand offers a unique opportunity to link geophysical imaging of the subduction zone with direct access to incoming material that represents the megathrust fault rocks hosting slow slip. Two recent International Ocean Discovery Program Expeditions sampled this incoming material before it is entrained immediately down-dip along the shallow plate interface. Drilling results, tied to regional seismic reflection images, reveal heterogeneous lithologies with highly variable physical ...
At the northern Hikurangi margin (North Island, New Zealand), shallow slow slip events (SSEs) freque...
The northern Hikurangi subduction margin hosts slow slip events (SSEs), which are exceptionally shal...
Geophysical observations show spatial and temporal variations in fault slip style on shallow subduct...
Slow slip events (SSEs) accommodate a significant proportion of tectonic plate motion at subduction ...
Slow slip events (SSEs) are recognized as an important component of plate boundary fault slip, and t...
Recent geodetic studies have shown that slow-slip events can occur on subduction faults, including t...
Slow slip events are well documented in global subduction zones at depths of 30–50 km. Tectonic (non...
Slow slip events are well documented in global subduction zones at depths of 30-50 km. Tectoni...
Slow slip events (SSEs) involve episodic transient fault slip of millimetres to tens of centimetres ...
Fluid migration and pore fluid pressure have been implicated in generating the transitional fault zo...
Slow slip events (SSEs) are interpreted as the transient quasi-static fault deformation in the deep ...
We use a prestack depth migration reflection image and magnetic anomaly data across the northern Hik...
Slow slip events (SSEs) at the northern Hikurangi subduction margin, New Zealand, are among the best...
Slow slip events (SSEs) at the northern Hikurangi subduction margin, New Zealand, are among the best...
We investigated the seismic velocity structure of the Hikurangi margin in New Zealand to uncover the...
At the northern Hikurangi margin (North Island, New Zealand), shallow slow slip events (SSEs) freque...
The northern Hikurangi subduction margin hosts slow slip events (SSEs), which are exceptionally shal...
Geophysical observations show spatial and temporal variations in fault slip style on shallow subduct...
Slow slip events (SSEs) accommodate a significant proportion of tectonic plate motion at subduction ...
Slow slip events (SSEs) are recognized as an important component of plate boundary fault slip, and t...
Recent geodetic studies have shown that slow-slip events can occur on subduction faults, including t...
Slow slip events are well documented in global subduction zones at depths of 30–50 km. Tectonic (non...
Slow slip events are well documented in global subduction zones at depths of 30-50 km. Tectoni...
Slow slip events (SSEs) involve episodic transient fault slip of millimetres to tens of centimetres ...
Fluid migration and pore fluid pressure have been implicated in generating the transitional fault zo...
Slow slip events (SSEs) are interpreted as the transient quasi-static fault deformation in the deep ...
We use a prestack depth migration reflection image and magnetic anomaly data across the northern Hik...
Slow slip events (SSEs) at the northern Hikurangi subduction margin, New Zealand, are among the best...
Slow slip events (SSEs) at the northern Hikurangi subduction margin, New Zealand, are among the best...
We investigated the seismic velocity structure of the Hikurangi margin in New Zealand to uncover the...
At the northern Hikurangi margin (North Island, New Zealand), shallow slow slip events (SSEs) freque...
The northern Hikurangi subduction margin hosts slow slip events (SSEs), which are exceptionally shal...
Geophysical observations show spatial and temporal variations in fault slip style on shallow subduct...