{"@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/1360004233292223744.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2018jb016136"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018JB016136"}},{"identifier":{"@type":"URI","@value":"http://api.wiley.com/onlinelibrary/chorus/v1/articles/10.1029%2F2018JB016136"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB016136"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Earthquakes and Tremor Linked to Seamount Subduction During Shallow Slow Slip at the Hikurangi Margin, New Zealand"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Shallow slow slip events have been well documented offshore Gisborne at the northern Hikurangi subduction margin, New Zealand, and are associated with tectonic tremor downdip of the slow slip patch and increases in local microseismicity. Tremor and seismicity on the shallow subduction interface are often poorly resolved due to their distance from land‐based seismic and geodetic networks. To address this shortcoming, the Hikurangi Ocean Bottom Investigation of Tremor and Slow Slip experiment deployed 24 absolute pressure gauges and 15 ocean bottom seismometers on the seafloor above the Gisborne slow slip patch to investigate the spatial and temporal extent of slow slip and associated tremor and earthquake activity. We present a detailed spatiotemporal analysis of the seismic signatures of various interplate slip processes associated with the September/October 2014 Gisborne slow slip event. Tectonic tremor begins toward the end and continues after the geodetically constrained slow slip event and is localized in the vicinity of two subducted seamounts within and updip of the slow slip patch. The subsequent, rather than synchronous occurrence of tremor suggests that tremor may be triggered by stress changes induced by slow slip. However, Coulomb failure stress change models based on the slow slip distribution fail to predict the location of tremor, suggesting that seamount subduction plays a dominant role in the stress state of the shallow megathrust. This and the observed interplay of seismic and aseismic interplate slip processes imply that stress changes from slow slip play a secondary role in the distribution of associated microseismicity.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004233292223760","@type":"Researcher","foaf:name":[{"@value":"Erin K. Todd"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Sciences University of California Santa Cruz CA USA"},{"@value":"Now at Department of Geology University of Otago Dunedin New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233292224007","@type":"Researcher","foaf:name":[{"@value":"Susan Y. Schwartz"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Sciences University of California Santa Cruz CA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801212570752","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"80292861"},{"@type":"NRID","@value":"1000080292861"},{"@type":"NRID","@value":"9000001755202"},{"@type":"NRID","@value":"9000024177914"},{"@type":"NRID","@value":"9000264263201"},{"@type":"NRID","@value":"9000000236437"},{"@type":"NRID","@value":"9000237782980"},{"@type":"NRID","@value":"9000014139694"},{"@type":"NRID","@value":"9000256898269"},{"@type":"NRID","@value":"9000256898282"},{"@type":"NRID","@value":"9000020071144"},{"@type":"NRID","@value":"9000405704131"},{"@type":"NRID","@value":"9000014692993"},{"@type":"NRID","@value":"9000347166248"},{"@type":"NRID","@value":"9000237783564"},{"@type":"NRID","@value":"9000254741850"},{"@type":"NRID","@value":"9000258737404"},{"@type":"NRID","@value":"9000382634130"},{"@type":"NRID","@value":"9000254741043"},{"@type":"NRID","@value":"9000375915029"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0196034"}],"foaf:name":[{"@value":"Kimihiro Mochizuki"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute University of Tokyo Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233292223621","@type":"Researcher","foaf:name":[{"@value":"Laura M. Wallace"}],"jpcoar:affiliationName":[{"@value":"GNS Science Lower Hutt New Zealand"},{"@value":"University of Texas Institute for Geophysics (UTIG) Austin TX USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233292224005","@type":"Researcher","foaf:name":[{"@value":"Anne F. Sheehan"}],"jpcoar:affiliationName":[{"@value":"Cooperative Institute for Research in Environmental Sciences University of Colorado Boulder Boulder CO USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233292223744","@type":"Researcher","foaf:name":[{"@value":"Spahr C. Webb"}],"jpcoar:affiliationName":[{"@value":"Lamont‐Doherty Earth Observatory (LDEO) Columbia University New York NY USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233292224011","@type":"Researcher","foaf:name":[{"@value":"Charles A. Williams"}],"jpcoar:affiliationName":[{"@value":"GNS Science Lower Hutt New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233292223768","@type":"Researcher","foaf:name":[{"@value":"Jenny Nakai"}],"jpcoar:affiliationName":[{"@value":"Cooperative Institute for Research in Environmental Sciences University of Colorado Boulder Boulder CO USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233292223620","@type":"Researcher","foaf:name":[{"@value":"Jefferson Yarce"}],"jpcoar:affiliationName":[{"@value":"Cooperative Institute for Research in Environmental Sciences University of Colorado Boulder Boulder CO USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233292223493","@type":"Researcher","foaf:name":[{"@value":"Bill Fry"}],"jpcoar:affiliationName":[{"@value":"GNS Science Lower Hutt New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233292223878","@type":"Researcher","foaf:name":[{"@value":"Stuart Henrys"}],"jpcoar:affiliationName":[{"@value":"GNS Science Lower Hutt New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1420564276172946176","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"30435581"},{"@type":"NRID","@value":"1000030435581"},{"@type":"ORCID","@value":"0000-0001-9484-9539"},{"@type":"CINII_AUTHOR_ID","@value":"DA17240097"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA17240097#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA17240097"},{"@type":"NRID","@value":"9000002327811"},{"@type":"NRID","@value":"9000254263259"},{"@type":"NRID","@value":"9000254741331"},{"@type":"NRID","@value":"9000001755219"},{"@type":"NRID","@value":"9000001756269"},{"@type":"NRID","@value":"9000413695854"},{"@type":"NRID","@value":"9000254263251"},{"@type":"NRID","@value":"9000412206699"},{"@type":"NRID","@value":"9000283726644"},{"@type":"NRID","@value":"9000258283045"},{"@type":"NRID","@value":"9000380434917"},{"@type":"NRID","@value":"9000410949101"},{"@type":"NRID","@value":"9000016847657"},{"@type":"NRID","@value":"9000347135736"},{"@type":"NRID","@value":"9000391404808"},{"@type":"NRID","@value":"9000347166246"},{"@type":"NRID","@value":"9000006894368"},{"@type":"NRID","@value":"9000347135626"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0134551"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/YoshihiroIto"}],"foaf:name":[{"@value":"Yoshihiro Ito"}],"jpcoar:affiliationName":[{"@value":"Disaster Prevention Research Institute Kyoto University Kyoto Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"21699313"},{"@type":"EISSN","@value":"21699356"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2018-08","prism:volume":"123","prism:number":"8","prism:startingPage":"6769","prism:endingPage":"6783"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018JB016136"},{"@id":"http://api.wiley.com/onlinelibrary/chorus/v1/articles/10.1029%2F2018JB016136"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB016136"}],"createdAt":"2018-07-27","modifiedAt":"2024-07-08","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781902844800","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H06475"},{"@type":"JGN","@value":"JP16H06475"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-16H06475/"}],"notation":[{"@language":"ja","@value":"スロー地震発生領域周辺の地震学的・電磁気学的構造の解明"},{"@language":"en","@value":"Study on Seismic and Electromagnetic Subsurface Structure around the Source of Slow Earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256879576576","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H06476"},{"@type":"JGN","@value":"JP16H06476"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-16H06476/"}],"notation":[{"@language":"ja","@value":"スロー地震の地質学的描像と摩擦・水理特性の解明"},{"@language":"en","@value":"Study on geological perspectives, frictional and hydrological properties of slow earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257259871104","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26257206"},{"@type":"JGN","@value":"JP26257206"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26257206/"}],"notation":[{"@language":"ja","@value":"沈み込み帯浅部のスロースリップはトラフ軸まで到達するか？"},{"@language":"en","@value":"Slow slip to the trench  ?"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050009295028707584","@type":"Article","resourceType":"学術雑誌論文(journal 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Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094768581248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The dammed Hikurangi Trough: a channel‐fed trench blocked by subducting seamounts and their wake avalanches (New Zealand–France GeodyNZ Project)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096173467776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Large-scale dynamic triggering of shallow slow slip enhanced by overlying sedimentary wedge"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118672522880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial relationship between shallow very low frequency earthquakes and the subducted Kyushu-Palau Ridge in the Hyuga-nada region of the Nankai subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580230600319872","@type":"Article","resourceType":"学術雑誌論文(journal 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