Abstract
Following the 2016 Mw 7.8 Kaikoura earthquake, uncertainty over the nature of the coseismic rupture developed. Seismological evidence pointed to significant involvement of the subduction megathrust, while geodetic and field observations pointed to a shallow set of intracrustal faults as the main participants during the earthquake. The addition of tsunami observations and modeling as reported in Bai et al. (2017) places additional constraints on the specific location of coseismic slip, which when combined with other observations indicates the simultaneous occurrence of shallow slip on the subduction interface and slip on overlying, upper crustal fault structures. This Kaikoura-style earthquake, involving synchronous ruptures on multiple components of the plate boundary, is an important mode of plate boundary deformation affecting seismic hazard along subduction zones.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 6788-6791 |
| Number of pages | 4 |
| Journal | Geophysical Research Letters |
| Volume | 44 |
| Issue number | 13 |
| DOIs |
|
| State | Published - Jul 16 2017 |
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All Science Journal Classification (ASJC) codes
- Geophysics
- Earth and Planetary Sciences(all)
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Reconciling the deformational dichotomy of the 2016 Mw 7.8 Kaikoura New Zealand earthquake. / Furlong, Kevin Patrick; Herman, Matthew.
In: Geophysical Research Letters, Vol. 44, No. 13, 16.07.2017, p. 6788-6791.Research output: Contribution to journal › Comment/debate
TY - JOUR
T1 - Reconciling the deformational dichotomy of the 2016 Mw 7.8 Kaikoura New Zealand earthquake
AU - Furlong, Kevin Patrick
AU - Herman, Matthew
PY - 2017/7/16
Y1 - 2017/7/16
N2 - Following the 2016 Mw 7.8 Kaikoura earthquake, uncertainty over the nature of the coseismic rupture developed. Seismological evidence pointed to significant involvement of the subduction megathrust, while geodetic and field observations pointed to a shallow set of intracrustal faults as the main participants during the earthquake. The addition of tsunami observations and modeling as reported in Bai et al. (2017) places additional constraints on the specific location of coseismic slip, which when combined with other observations indicates the simultaneous occurrence of shallow slip on the subduction interface and slip on overlying, upper crustal fault structures. This Kaikoura-style earthquake, involving synchronous ruptures on multiple components of the plate boundary, is an important mode of plate boundary deformation affecting seismic hazard along subduction zones.
AB - Following the 2016 Mw 7.8 Kaikoura earthquake, uncertainty over the nature of the coseismic rupture developed. Seismological evidence pointed to significant involvement of the subduction megathrust, while geodetic and field observations pointed to a shallow set of intracrustal faults as the main participants during the earthquake. The addition of tsunami observations and modeling as reported in Bai et al. (2017) places additional constraints on the specific location of coseismic slip, which when combined with other observations indicates the simultaneous occurrence of shallow slip on the subduction interface and slip on overlying, upper crustal fault structures. This Kaikoura-style earthquake, involving synchronous ruptures on multiple components of the plate boundary, is an important mode of plate boundary deformation affecting seismic hazard along subduction zones.
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U2 - 10.1002/2017GL074365
DO - 10.1002/2017GL074365
M3 - Comment/debate
AN - SCOPUS:85021702877
VL - 44
SP - 6788
EP - 6791
JO - Geophysical Research Letters
JF - Geophysical Research Letters
SN - 0094-8276
IS - 13
ER -