Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/78511
Title: Transpressional rupture cascade of the 2016 m-w 7.8 Kaikoura earthquake, New Zealand
Authors: Xu, WB 
Feng, GC
Meng, LS
Zhang, AL
Ampuero, JP
Burgmann, R
Fang, LH
Keywords: Kaikoura earthquake
Geodetic slip
Back projection
InSAR 3-D displacement
Issue Date: 2018
Publisher: John Wiley & Sons
Source: Journal of geophysical research. B, Solid earth, Mar. 2018, v. 123, no. 3, p. 2396-2409 How to cite?
Journal: Journal of geophysical research. B, Solid earth 
Abstract: Large earthquakes often do not occur on a simple planar fault but involve rupture of multiple geometrically complex faults. The 2016 M-w 7.8 Kaikoura earthquake, New Zealand, involved the rupture of at least 21 faults, propagating from southwest to northeast for about 180km. Here we combine space geodesy and seismology techniques to study subsurface fault geometry, slip distribution, and the kinematics of the rupture. Our finite-fault slip model indicates that the fault motion changes from predominantly right-lateral slip near the epicenter to transpressional slip in the northeast with a maximum coseismic surface displacement of about 10m near the intersection between the Kekerengu and Papatea faults. Teleseismic back projection imaging shows that rupture speed was overall slow (1.4km/s) but faster on individual fault segments (approximately 2km/s) and that the conjugate, oblique-reverse, north striking faults released the largest high-frequency energy. We show that the linking Conway-Charwell faults aided in propagation of rupture across the step over from the Humps fault zone to the Hope fault. Fault slip cascaded along the Jordan Thrust, Kekerengu, and Needles faults, causing stress perturbations that activated two major conjugate faults, the Hundalee and Papatea faults. Our results shed important light on the study of earthquakes and seismic hazard evaluation in geometrically complex fault systems.
URI: http://hdl.handle.net/10397/78511
ISSN: 2169-9313
EISSN: 2169-9356
DOI: 10.1002/2017JB015168
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