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Two regions of seafloor deformation generated the tsunami for the 13 November 2016, Kaikoura, New Zealand earthquake
The 13 November 2016 Kaikoura, New Zealand, Mw 7.8 earthquake ruptured multiple crustal faults in the transpressional Marlborough and North Canterbury tectonic domains of northeastern South Island. The Hikurangi trench and underthrust Pacific slab terminate in the region south of Kaikoura, as the su...
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Published in: | Geophysical research letters 2017-07, Vol.44 (13), p.6597-6606 |
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description | The 13 November 2016 Kaikoura, New Zealand, Mw 7.8 earthquake ruptured multiple crustal faults in the transpressional Marlborough and North Canterbury tectonic domains of northeastern South Island. The Hikurangi trench and underthrust Pacific slab terminate in the region south of Kaikoura, as the subdution zone transitions to the Alpine fault strike‐slip regime. It is difficult to establish whether any coseismic slip occurred on the megathrust from on‐land observations. The rupture generated a tsunami well recorded at tide gauges along the eastern coasts and in Chatham Islands, including a ~4 m crest‐to‐trough signal at Kaikoura where coastal uplift was about 1 m, and at multiple gauges in Wellington Harbor. Iterative modeling of teleseismic body waves and the regional water‐level recordings establishes that two regions of seafloor motion produced the tsunami, including an Mw ~7.6 rupture on the megathrust below Kaikoura and comparable size transpressional crustal faulting extending offshore near Cook Strait.
Key Points
The 2016 Kaikoura earthquake produced tsunami signals that indicate sizeable seafloor deformation in addition to onshore surface ruptures
Iterative modeling of teleseismic P and SH waves and regional tide and wave gauge recordings indicates two regions of seafloor deformation
Tsunami excitation involved oblique thrusting on the southern Hikurangi megathrust and offshore extension of transpressional faults |
doi_str_mv | 10.1002/2017GL073717 |
format | article |
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Key Points
The 2016 Kaikoura earthquake produced tsunami signals that indicate sizeable seafloor deformation in addition to onshore surface ruptures
Iterative modeling of teleseismic P and SH waves and regional tide and wave gauge recordings indicates two regions of seafloor deformation
Tsunami excitation involved oblique thrusting on the southern Hikurangi megathrust and offshore extension of transpressional faults</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1002/2017GL073717</identifier><language>eng</language><publisher>Washington: John Wiley & Sons, Inc</publisher><subject>Body waves ; Coastal environments ; Deformation ; Earthquake ; Earthquakes ; Fault lines ; Faults ; Gauges ; Geological faults ; Harbors ; Hikurangi subduction zone ; Islands ; Iterative methods ; Measuring instruments ; Modelling ; Ocean floor ; Offshore ; Regions ; Rupture ; Rupturing ; Seismic activity ; Slip ; Tide gauges ; Tides ; Trenches (pipelines) ; Tsunami ; Tsunamis ; Uplift ; Water levels</subject><ispartof>Geophysical research letters, 2017-07, Vol.44 (13), p.6597-6606</ispartof><rights>2017. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a4334-2ba5d045a7d741377af7ce9a30eb829b1be113d99441ebccb65eec7e1a0449e43</citedby><cites>FETCH-LOGICAL-a4334-2ba5d045a7d741377af7ce9a30eb829b1be113d99441ebccb65eec7e1a0449e43</cites><orcidid>0000-0003-2360-4213 ; 0000-0002-8739-2072 ; 0000-0003-3323-3348 ; 0000-0002-7435-0500</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2F2017GL073717$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2F2017GL073717$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,11514,27924,27925,46468,46892</link.rule.ids></links><search><creatorcontrib>Bai, Yefei</creatorcontrib><creatorcontrib>Lay, Thorne</creatorcontrib><creatorcontrib>Cheung, Kwok Fai</creatorcontrib><creatorcontrib>Ye, Lingling</creatorcontrib><title>Two regions of seafloor deformation generated the tsunami for the 13 November 2016, Kaikoura, New Zealand earthquake</title><title>Geophysical research letters</title><description>The 13 November 2016 Kaikoura, New Zealand, Mw 7.8 earthquake ruptured multiple crustal faults in the transpressional Marlborough and North Canterbury tectonic domains of northeastern South Island. The Hikurangi trench and underthrust Pacific slab terminate in the region south of Kaikoura, as the subdution zone transitions to the Alpine fault strike‐slip regime. It is difficult to establish whether any coseismic slip occurred on the megathrust from on‐land observations. The rupture generated a tsunami well recorded at tide gauges along the eastern coasts and in Chatham Islands, including a ~4 m crest‐to‐trough signal at Kaikoura where coastal uplift was about 1 m, and at multiple gauges in Wellington Harbor. Iterative modeling of teleseismic body waves and the regional water‐level recordings establishes that two regions of seafloor motion produced the tsunami, including an Mw ~7.6 rupture on the megathrust below Kaikoura and comparable size transpressional crustal faulting extending offshore near Cook Strait.
Key Points
The 2016 Kaikoura earthquake produced tsunami signals that indicate sizeable seafloor deformation in addition to onshore surface ruptures
Iterative modeling of teleseismic P and SH waves and regional tide and wave gauge recordings indicates two regions of seafloor deformation
Tsunami excitation involved oblique thrusting on the southern Hikurangi megathrust and offshore extension of transpressional faults</description><subject>Body waves</subject><subject>Coastal environments</subject><subject>Deformation</subject><subject>Earthquake</subject><subject>Earthquakes</subject><subject>Fault lines</subject><subject>Faults</subject><subject>Gauges</subject><subject>Geological faults</subject><subject>Harbors</subject><subject>Hikurangi subduction zone</subject><subject>Islands</subject><subject>Iterative methods</subject><subject>Measuring instruments</subject><subject>Modelling</subject><subject>Ocean floor</subject><subject>Offshore</subject><subject>Regions</subject><subject>Rupture</subject><subject>Rupturing</subject><subject>Seismic activity</subject><subject>Slip</subject><subject>Tide gauges</subject><subject>Tides</subject><subject>Trenches (pipelines)</subject><subject>Tsunami</subject><subject>Tsunamis</subject><subject>Uplift</subject><subject>Water levels</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNp9kEFPwzAMhSMEEmNw4wdE4rqC06TNekQTDMQ0JDQuXCq3dbdubbMlLdP-PYFx4MTJtt4n-_kxdi3gVgCEdyEIPZ2BllroEzYQiVLBGECfsgFA4vtQx-fswrk1AEiQYsC6xd5wS8vKtI6bkjvCsjbG8oJKYxvsvMCX1JLFjgrerYh3rm-xqbjXf2Yh-dx8UpOR5d5BPOIvWG1Mb3HE57TnH4Q1tgUntN1q1-OGLtlZibWjq986ZO-PD4vJUzB7nT5P7mcBKilVEGYYFaAi1IVWQmqNpc4pQQmUjcMkExkJIYvEvykoy_MsjohyTQJBqYSUHLKb496tNbueXJeuva3Wn0xFEoZJJCOpPTU6Urk1zlkq062tGrSHVED6nWv6N1ePh0d8X9V0-JdNp2-zKAat5BegcXiW</recordid><startdate>20170716</startdate><enddate>20170716</enddate><creator>Bai, Yefei</creator><creator>Lay, Thorne</creator><creator>Cheung, Kwok Fai</creator><creator>Ye, Lingling</creator><general>John Wiley & Sons, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>8FD</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><orcidid>https://orcid.org/0000-0003-2360-4213</orcidid><orcidid>https://orcid.org/0000-0002-8739-2072</orcidid><orcidid>https://orcid.org/0000-0003-3323-3348</orcidid><orcidid>https://orcid.org/0000-0002-7435-0500</orcidid></search><sort><creationdate>20170716</creationdate><title>Two regions of seafloor deformation generated the tsunami for the 13 November 2016, Kaikoura, New Zealand earthquake</title><author>Bai, Yefei ; Lay, Thorne ; Cheung, Kwok Fai ; Ye, Lingling</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a4334-2ba5d045a7d741377af7ce9a30eb829b1be113d99441ebccb65eec7e1a0449e43</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Body waves</topic><topic>Coastal environments</topic><topic>Deformation</topic><topic>Earthquake</topic><topic>Earthquakes</topic><topic>Fault lines</topic><topic>Faults</topic><topic>Gauges</topic><topic>Geological faults</topic><topic>Harbors</topic><topic>Hikurangi subduction zone</topic><topic>Islands</topic><topic>Iterative methods</topic><topic>Measuring instruments</topic><topic>Modelling</topic><topic>Ocean floor</topic><topic>Offshore</topic><topic>Regions</topic><topic>Rupture</topic><topic>Rupturing</topic><topic>Seismic activity</topic><topic>Slip</topic><topic>Tide gauges</topic><topic>Tides</topic><topic>Trenches (pipelines)</topic><topic>Tsunami</topic><topic>Tsunamis</topic><topic>Uplift</topic><topic>Water levels</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bai, Yefei</creatorcontrib><creatorcontrib>Lay, Thorne</creatorcontrib><creatorcontrib>Cheung, Kwok Fai</creatorcontrib><creatorcontrib>Ye, Lingling</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Technology Research Database</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bai, Yefei</au><au>Lay, Thorne</au><au>Cheung, Kwok Fai</au><au>Ye, Lingling</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Two regions of seafloor deformation generated the tsunami for the 13 November 2016, Kaikoura, New Zealand earthquake</atitle><jtitle>Geophysical research letters</jtitle><date>2017-07-16</date><risdate>2017</risdate><volume>44</volume><issue>13</issue><spage>6597</spage><epage>6606</epage><pages>6597-6606</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><abstract>The 13 November 2016 Kaikoura, New Zealand, Mw 7.8 earthquake ruptured multiple crustal faults in the transpressional Marlborough and North Canterbury tectonic domains of northeastern South Island. The Hikurangi trench and underthrust Pacific slab terminate in the region south of Kaikoura, as the subdution zone transitions to the Alpine fault strike‐slip regime. It is difficult to establish whether any coseismic slip occurred on the megathrust from on‐land observations. The rupture generated a tsunami well recorded at tide gauges along the eastern coasts and in Chatham Islands, including a ~4 m crest‐to‐trough signal at Kaikoura where coastal uplift was about 1 m, and at multiple gauges in Wellington Harbor. Iterative modeling of teleseismic body waves and the regional water‐level recordings establishes that two regions of seafloor motion produced the tsunami, including an Mw ~7.6 rupture on the megathrust below Kaikoura and comparable size transpressional crustal faulting extending offshore near Cook Strait.
Key Points
The 2016 Kaikoura earthquake produced tsunami signals that indicate sizeable seafloor deformation in addition to onshore surface ruptures
Iterative modeling of teleseismic P and SH waves and regional tide and wave gauge recordings indicates two regions of seafloor deformation
Tsunami excitation involved oblique thrusting on the southern Hikurangi megathrust and offshore extension of transpressional faults</abstract><cop>Washington</cop><pub>John Wiley & Sons, Inc</pub><doi>10.1002/2017GL073717</doi><tpages>10</tpages><orcidid>https://orcid.org/0000-0003-2360-4213</orcidid><orcidid>https://orcid.org/0000-0002-8739-2072</orcidid><orcidid>https://orcid.org/0000-0003-3323-3348</orcidid><orcidid>https://orcid.org/0000-0002-7435-0500</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Body waves Coastal environments Deformation Earthquake Earthquakes Fault lines Faults Gauges Geological faults Harbors Hikurangi subduction zone Islands Iterative methods Measuring instruments Modelling Ocean floor Offshore Regions Rupture Rupturing Seismic activity Slip Tide gauges Tides Trenches (pipelines) Tsunami Tsunamis Uplift Water levels |
title | Two regions of seafloor deformation generated the tsunami for the 13 November 2016, Kaikoura, New Zealand earthquake |
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