{"@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/1360005518173396992.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2019jb017988"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2019JB017988"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019JB017988"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2019JB017988"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019JB017988"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Comprehensive Detection of Very Low Frequency Earthquakes Off the Hokkaido and Tohoku Pacific Coasts, Northeastern Japan"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Very low frequency earthquakes (VLFEs), classified as one type of slow earthquake, occur near seismogenic zones and can be a proxy for interplate slow slip. We investigated VLFE activity off the Hokkaido and Tohoku Pacific coasts, where the Pacific plate subducts under the North American plate. Comprehensive detection of VLFEs is performed for the period from January 2003 to July 2018 by a matched‐filter technique utilizing synthetic waveforms calculated based on a three‐dimensional velocity structure model. The spatiotemporal consistency between the afterslip of the 2003 Tokachi‐Oki earthquake (Mw 8.0) and VLFE distribution off the Hokkaido coast suggests that VLFE activity can reflect interplate slow slip. Inside a large coseismic slip area of the 2011 Tohoku earthquake (Mw 9.0), the VLFE activity was low thereafter, whereas outside the area, VLFE activity increased after the 2011 Tohoku earthquake. These characteristics are consistent with aseismic slip distributions estimated from repeating earthquakes. VLFEs were sometimes activated by afterslips of interplate earthquakes with Mw of 6–7, such as the 2008 Fukushima‐Oki earthquake and aftershocks of the 2011 Tohoku earthquake. Even in the coseismic slip areas of very large earthquakes, we found the occurrence of episodic bursts every 3 months to a year during an interseismic period between very large earthquakes. Such VLFE bursts may suggest small slips during the interseismic period.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380005518173397120","@type":"Researcher","foaf:name":[{"@value":"Satoru Baba"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute The University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173396993","@type":"Researcher","foaf:name":[{"@value":"Akiko Takeo"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute The University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173396992","@type":"Researcher","foaf:name":[{"@value":"Kazushige Obara"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute The University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173396864","@type":"Researcher","foaf:name":[{"@value":"Takanori Matsuzawa"}],"jpcoar:affiliationName":[{"@value":"National Research Institute for Earth Science and Disaster Resilience  Ibaraki Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173396994","@type":"Researcher","foaf:name":[{"@value":"Takuto Maeda"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Science and Technology Hirosaki University  Aomori 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":"2020-01","prism:volume":"125","prism:number":"1","prism:startingPage":"e2019JB017988"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2019JB017988"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019JB017988"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2019JB017988"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019JB017988"}],"createdAt":"2019-12-21","modifiedAt":"2023-09-04","project":[{"@id":"https://cir.nii.ac.jp/crid/1040003825673935488","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"19J20760"},{"@type":"JGN","@value":"JP19J20760"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-19J20760/"}],"notation":[{"@language":"ja","@value":"スロー地震の新たな検出手法の開発とそれに基づく比較沈み込み帯学の構築"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202761516800","@type":"Article","resourceType":"学術雑誌論文(journal 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Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269991901952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slow Earthquakes Coincident with Episodic Tremors and Slow Slip Events"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512426624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Recent progress of seismic observation networks in Japan"},{"@value":"Recent progress of seismic observation networks in Japan--Hi-net, F-net, K-NET and KiK-net"},{"@value":"Recent progress of seismic observation networks in Japan —Hi-net, F-net, K-NET and KiK-net—"},{"@value":"Recent progress of seismic observation networks in Japan—Hi-net, F-net, K-NET and KiK-net"},{"@value":"Recent progress of seismic observation networks in Japan—Hi‐net, F‐net, K‐NET and KiK‐net—"},{"@value":"Recent progress of seismic observation networks in Japan–Hi-net, F-net, K-net and KiK-net—"},{"@value":"Recent progress of seismic observation network in Japan --H-net, F-net, K-NET and KiK-net"},{"@value":"Recent progress of seismic observation networks in Japan⿢Hi-net and F-net and K-NET and KiK-net"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512583680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Very low frequency earthquakes excited by the 2004 off the Kii peninsula earthquakes: A dynamic deformation process in the large accretionary prism"},{"@value":"Very low frequency earthquake excited by the 2004 off the Kii peninsula earthquake: a dynamic deformation process in the large accretionary prism"},{"@value":"Very low frequency earthquakes excited by the 2004 off Kii peninsula earthquakes: a dynamic deformation process in the large accretionary prism"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489915520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source rupture process of the 2003 Tokachi-oki earthquake determined by joint inversion of teleseismic body wave and strong ground motion data"},{"@value":"Rupture process of the 2016 Kumamoto earthquake in relation to the thermal structure around Aso volcano"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489922688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Low frequency events occurred during the sequence of aftershock activity of the 2003 Tokachi-Oki earthquake; a dynamic process of the tectonic erosion by subducted seamount"}]},{"@id":"https://cir.nii.ac.jp/crid/1390567172587194752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Errata to “Characteristic activities of slow earthquakes in Japan”"},{"@value":"Characteristic activities of slow earthquakes in 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