{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361699994805576448.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2018gl077385"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2018GL077385"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2018GL077385"}}],"dc:title":[{"@value":"Triggered Slow Slip and Afterslip on the Southern Hikurangi Subduction Zone Following the Kaikōura Earthquake"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The 2016 M<jats:sub>W</jats:sub>7.8 Kaikōura earthquake ruptured a complex sequence of strike‐slip and reverse faults in New Zealand's northeastern South Island. In the months following the earthquake, time‐dependent inversions of Global Positioning System and interferometric synthetic aperture radar data reveal up to 0.5 m of afterslip on the subduction interface beneath the northern South Island underlying the crustal faults that ruptured in the earthquake. This is clear evidence that the far southern end of the Hikurangi subduction zone accommodates plate motion. The M<jats:sub>W</jats:sub>7.8 earthquake also triggered widespread slow slip over much of the subduction zone beneath the North Island. The triggered slow slip included immediate triggering of shallow (<15 km), short (2–3 weeks) slow slip events along much of the east coast, and deep (>30 km), long‐term (>1 year) slow slip beneath the southern North Island. The southern Hikurangi slow slip was likely triggered by large (0.5–1.0 MPa) static Coulomb stress increases.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699994805576448","@type":"Researcher","foaf:name":[{"@value":"Laura M. Wallace"}],"jpcoar:affiliationName":[{"@value":"GNS Science  Lower Hutt New Zealand"},{"@value":"Institute for Geophysics University of Texas at Austin  Austin TX USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994805576452","@type":"Researcher","foaf:name":[{"@value":"Sigrún Hreinsdóttir"}],"jpcoar:affiliationName":[{"@value":"GNS Science  Lower Hutt New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994805576449","@type":"Researcher","foaf:name":[{"@value":"Susan Ellis"}],"jpcoar:affiliationName":[{"@value":"GNS Science  Lower Hutt New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994805576451","@type":"Researcher","foaf:name":[{"@value":"Ian Hamling"}],"jpcoar:affiliationName":[{"@value":"GNS Science  Lower Hutt New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994805576450","@type":"Researcher","foaf:name":[{"@value":"Elisabetta D'Anastasio"}],"jpcoar:affiliationName":[{"@value":"GNS Science  Lower Hutt New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994805576453","@type":"Researcher","foaf:name":[{"@value":"Paul Denys"}],"jpcoar:affiliationName":[{"@value":"Surveying School University of Otago  Dunedin New Zealand"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2018-05-21","prism:volume":"45","prism:number":"10","prism:startingPage":"4710","prism:endingPage":"4718"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2018GL077385"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2018GL077385"}],"createdAt":"2018-03-31","modifiedAt":"2023-09-02","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360017282189362304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Crustal Structure of the Hikurangi Margin From SHIRE Seismic Data and the Relationship Between Forearc Structure and Shallow Megathrust Slip Behavior"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282189457792","@type":"Article","resourceType":"学術雑誌論文(journal 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