Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/106351
Full metadata record
DC FieldValueLanguage
dc.contributor.authorWang, Tengen
dc.contributor.authorWei, Shengjien
dc.contributor.authorShi, Xuhuaen
dc.contributor.authorQiu, Qiangen
dc.contributor.authorLi, Linlinen
dc.contributor.authorPeng, Dongjuen
dc.contributor.authorWeldon, Ray J.en
dc.contributor.authorBarbot, Sylvainen
dc.date.accessioned2019-08-07T08:45:12Zen
dc.date.accessioned2019-12-06T22:09:39Z-
dc.date.available2019-08-07T08:45:12Zen
dc.date.available2019-12-06T22:09:39Z-
dc.date.issued2017en
dc.identifier.citationWang, T., Wei, S., Shi, X., Qiu, Q., Li, L., Peng, D., . . . Barbot, S. (2018). The 2016 Kaikōura earthquake : simultaneous rupture of the subduction interface and overlying faults. Earth and Planetary Science Letters, 482, 44-51. doi:10.1016/j.epsl.2017.10.056en
dc.identifier.issn0012-821Xen
dc.identifier.urihttps://hdl.handle.net/10356/106351-
dc.identifier.urihttp://hdl.handle.net/10220/49585en
dc.description.abstractThe distribution of slip during an earthquake and how it propagates among faults in the subduction system play a major role in seismic and tsunami hazards, yet they are poorly understood because offshore observations are often lacking. Here we derive the slip distribution and rupture evolution during the 2016 Mw 7.9 Kaikōura (New Zealand) earthquake that reconcile the surface rupture, space geodetic measurements, seismological and tsunami waveform records. We use twelve fault segments, with eleven in the crust and one on the megathrust interface, to model the geodetic data and match the major features of the complex surface ruptures. Our modeling result indicates that a large portion of the moment is distributed on the subduction interface, making a significant contribution to the far field surface deformation and teleseismic body waves. The inclusion of local strong motion and teleseismic waveform data in the joint inversion reveals a unilateral rupture towards northeast with a relatively low averaged rupture speed of ∼1.5 km/s. The first 30 s of the rupture took place on the crustal faults with oblique slip motion and jumped between fault segments that have large differences in strike and dip. The peak moment release occurred at ∼65 s, corresponding to simultaneous rupture of both plate interface and the overlying splay faults with rake angle changes progressively from thrust to strike-slip. The slip on the Papatea fault produced more than 2 m of offshore uplift, making a major contribution to the tsunami at the Kaikōura station, while the northeastern end of the rupture can explain the main features at the Wellington station. Our inversions and simulations illuminate complex up-dip rupture behavior that should be taken into consideration in both seismic and tsunami hazard assessment. The extreme complex rupture behavior also brings new challenges to the earthquake dynamic simulations and understanding the physics of earthquakes.en
dc.description.sponsorshipNRF (Natl Research Foundation, S’pore)en
dc.description.sponsorshipMOE (Min. of Education, S’pore)en
dc.format.extent8 p.en
dc.language.isoenen
dc.relation.ispartofseriesEarth and Planetary Science Lettersen
dc.rights© 2017 The Author(s). Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).en
dc.subjectFinite Rupture Modelen
dc.subjectStrong Motionen
dc.subjectSocial sciences::Geographyen
dc.titleThe 2016 Kaikōura earthquake : simultaneous rupture of the subduction interface and overlying faultsen
dc.typeJournal Articleen
dc.contributor.schoolAsian School of the Environmenten
dc.contributor.researchEarth Observatory of Singaporeen
dc.identifier.doi10.1016/j.epsl.2017.10.056en
dc.description.versionPublished versionen
item.fulltextWith Fulltext-
item.grantfulltextopen-
Appears in Collections:EOS Journal Articles

Google ScholarTM

Check

Altmetric


Plumx

Items in DR-NTU are protected by copyright, with all rights reserved, unless otherwise indicated.