scholarly journals Earthquakes triggered by slow slip at the plate interface in the Hikurangi subduction zone, New Zealand

2007 ◽  
Vol 34 (14) ◽  
Author(s):  
Martin Reyners ◽  
Stephen Bannister
Keyword(s):  
New Zealand ◽  
Subduction Zone ◽  
Slow Slip ◽  
Plate Interface

scholarly journals Slow slip near the trench at the Hikurangi subduction zone, New Zealand

Science ◽  
2016 ◽  
Vol 352 (6286) ◽  
pp. 701-704 ◽  
Author(s):  
L. M. Wallace ◽  
S. C. Webb ◽  
Y. Ito ◽  
K. Mochizuki ◽  
R. Hino ◽  
...  
Keyword(s):  
New Zealand ◽  
Subduction Zone ◽  
Slow Slip

Three‐Dimensional Modeling of Spontaneous and Triggered Slow‐Slip Events at the Hikurangi Subduction Zone, New Zealand

2019 ◽  
Vol 124 (12) ◽  
pp. 13250-13268 ◽  
Author(s):  
Bunichiro Shibazaki ◽  
Laura M. Wallace ◽  
Yoshihiro Kaneko ◽  
Ian Hamling ◽  
Yoshihiro Ito ◽  
...  
Keyword(s):  
New Zealand ◽  
Subduction Zone ◽  
Three Dimensional ◽  
Slow Slip ◽  
Slow Slip Events ◽  
Three Dimensional Modeling ◽  
Dimensional Modeling

Microseismicity but no tremor accompanying slow slip in the Hikurangi subduction zone, New Zealand

2009 ◽  
Vol 277 (1-2) ◽  
pp. 21-28 ◽  
Author(s):  
E.J. Delahaye ◽  
J. Townend ◽  
M.E. Reyners ◽  
G. Rogers
Keyword(s):  
New Zealand ◽  
Subduction Zone ◽  
Slow Slip

scholarly journals Seismicity and velocity structure in the vicinity of repeating slow slip earthquakes, northern Hikurangi subduction zone, New Zealand

2021 ◽  
Vol 563 ◽  
pp. 116887
Author(s):  
Kimihiro Mochizuki ◽  
Stuart Henrys ◽  
Daisuke Haijima ◽  
Emily Warren-Smith ◽  
Bill Fry
Keyword(s):  
New Zealand ◽  
Subduction Zone ◽  
Velocity Structure ◽  
Slow Slip

Slow Slip Events in New Zealand

2020 ◽  
Vol 48 (1) ◽  
pp. 175-203 ◽  
Author(s):  
Laura M. Wallace
Keyword(s):  
New Zealand ◽  
Subduction Zone ◽  
Slow Motion ◽  
Plate Motion ◽  
Slow Slip ◽  
Slow Slip Events ◽  
Diverse Range ◽  
The North ◽  
Interseismic Coupling ◽  
Natural Laboratory

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 zone. These slow slip events (SSEs) exhibit diverse characteristics, from shallow (<15 km), short (<1 month), frequent (every 1–2 years) events in the northern part of the subduction zone to deep (>30 km), long (>1 year), less frequent (approximately every 5 years) SSEs in the southern part of the subduction zone. Hikurangi SSEs show intriguing relationships to interseismic coupling, seismicity, and tectonic tremor, and they exhibit a diversity of interactions with large, regional earthquakes. Due to the marked along-strike variations in Hikurangi SSE characteristics, which coincide with changes in physical characteristics of the subduction margin, the Hikurangi subduction zone presents a globally unique natural laboratory to resolve outstanding questions regarding the origin of episodic, slow fault slip behavior. ▪  New Zealand's Hikurangi subduction zone hosts slow slip events with a diverse range of depth, size, duration, and recurrence characteristics. ▪  Hikurangi slow slip events show intriguing relationships with seismicity ranging from small earthquakes and tremor to larger earthquakes. ▪  Slow slip events play a major role in the accommodation of plate motion at the Hikurangi subduction zone. ▪  Many aspects of the Hikurangi subduction zone make it an ideal natural laboratory to resolve the physical processes controlling slow slip.

scholarly journals Observations of Laboratory and Natural Slow Slip Events: Hikurangi Subduction Zone, New Zealand

2020 ◽  
Vol 21 (2) ◽  
Author(s):  
Matt J. Ikari ◽  
Laura M. Wallace ◽  
Hannah S. Rabinowitz ◽  
Heather M. Savage ◽  
Ian J. Hamling ◽  
...  
Keyword(s):  
New Zealand ◽  
Subduction Zone ◽  
Slow Slip ◽  
Slow Slip Events
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