Slow slip events in New Zealand
LM Wallace - Annual Review of Earth and Planetary Sciences, 2020 - annualreviews.org
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 …
have revealed a diverse range of slow motion earthquakes on the Hikurangi subduction …
Characterizing the seismogenic zone of a major plate boundary subduction thrust: Hikurangi Margin, New Zealand
The Hikurangi subduction margin, New Zealand, has not experienced any significant (> Mw
7.2) subduction interface earthquakes since historical records began∼ 170 years ago …
7.2) subduction interface earthquakes since historical records began∼ 170 years ago …
Tectonic and geological framework for gas hydrates and cold seeps on the Hikurangi subduction margin, New Zealand
The imbricated frontal wedge of the central Hikurangi subduction margin is characteristic of
wide (ca. 150 km), poorly drained and over pressured, low taper (∼ 4°) thrust systems …
wide (ca. 150 km), poorly drained and over pressured, low taper (∼ 4°) thrust systems …
The volcanic, magmatic and tectonic setting of the Taupo Volcanic Zone, New Zealand, reviewed from a geothermal perspective
Abstract The Taupo Volcanic Zone (TVZ) in the North Island of New Zealand is one of the
world's most spectacular and productive areas of Quaternary silicic volcanism and …
world's most spectacular and productive areas of Quaternary silicic volcanism and …
The kinematics of a transition from subduction to strike‐slip: An example from the central New Zealand plate boundary
We develop a kinematic model for the transition from subduction beneath the North Island,
New Zealand, to strike‐slip in the South Island, constrained by GPS velocities and active …
New Zealand, to strike‐slip in the South Island, constrained by GPS velocities and active …
New Zealand Fault‐Rupture Depth Model v. 1.0: A Provisional Estimate of the Maximum Depth of Seismic Rupture on New Zealand's Active Faults
We summarize estimates of the maximum rupture depth on New Zealand's active faults
(“New Zealand Fault‐Rupture Depth Model v. 1.0”), as used in the New Zealand Community …
(“New Zealand Fault‐Rupture Depth Model v. 1.0”), as used in the New Zealand Community …
Two-phase Cretaceous–Paleocene rifting in the Taranaki Basin region, New Zealand; implications for Gondwana break-up
The break-up of Gondwana resulted in extension of New Zealand continental crust during
the Cretaceous–Paleocene. Offshore the geometry and rift history are well imaged by new …
the Cretaceous–Paleocene. Offshore the geometry and rift history are well imaged by new …
[LIVRE][B] Geology of the Rotorua area
GS Leonard, JG Begg, CJN Wilson, GS Leonard - 2010 - researchgate.net
1The QMAP Quaternary timescale pre-dates the presently recognised chronology for the
Pleistocene/Quaternary. QMAP adopted the Quaternary Period in 1994, based definitions on …
Pleistocene/Quaternary. QMAP adopted the Quaternary Period in 1994, based definitions on …
Regional structure and kinematic history of a large subduction back thrust: Taranaki Fault, New Zealand
The Taranaki Fault is a back thrust antithetic to the Hikurangi margin subduction thrust.
Subduction back thrusts, like the Taranaki Fault, accrue displacement transferred from the …
Subduction back thrusts, like the Taranaki Fault, accrue displacement transferred from the …
New perspectives on 'geological strain rates' calculated from both naturally deformed and actively deforming rocks
A value of∼ 10− 14 s− 1 is commonly cited as an average geological strain rate. This value
was first suggested for finite strain across an orogen, but based on more limited information …
was first suggested for finite strain across an orogen, but based on more limited information …