{"@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/1360005518172926208.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2019gl082448"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL082448"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2019GL082448"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL082448"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Structural Characteristics of the Nankai Trough Shallow Plate Boundary Inferred From Shallow Very Low Frequency Earthquakes"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The spatial distributions of shallow slow earthquakes are related to stress accumulation and structural characteristics of the shallow plate boundary, which are important for understanding megathrust earthquakes. To investigate spatiotemporal variation of shallow very low frequency earthquake (SVLFE) activity along the Nankai Trough, we conducted centroid moment tensor inversion method incorporating effects of offshore heterogeneous structures. By applying centroid moment tensor method into long‐term onshore seismograms, we obtained spatiotemporal variation of SVLFE activity occurred from June 2003 to May 2018. We find that SVLFE activities are related to the spatial variations of the slip‐deficit rate and pore fluid around the Philippine Sea plate boundary. SVLFEs are effectively activated by mechanical weakening due to rich pore fluid in areas surrounding strongly locked zones. Our results imply that spatial variations of long‐term SVLFE activity provide information on tectonic environments, which could constrain the rupture behavior of shallow plate boundaries during future megathrust earthquakes.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380005518172926208","@type":"Researcher","foaf:name":[{"@value":"Shunsuke Takemura"}],"jpcoar:affiliationName":[{"@value":"National Research Institute for Earth Science and Disaster Resilience  Tsukuba Japan"},{"@value":"Now at Earthquake Research Institute The University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518172926210","@type":"Researcher","foaf:name":[{"@value":"Takanori Matsuzawa"}],"jpcoar:affiliationName":[{"@value":"National Research Institute for Earth Science and Disaster Resilience  Tsukuba Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518172926211","@type":"Researcher","foaf:name":[{"@value":"Akemi Noda"}],"jpcoar:affiliationName":[{"@value":"National Research Institute for Earth Science and Disaster Resilience  Tsukuba Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518172926081","@type":"Researcher","foaf:name":[{"@value":"Takashi Tonegawa"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine‐Earth Science and Technology  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518172926080","@type":"Researcher","foaf:name":[{"@value":"Youichi Asano"}],"jpcoar:affiliationName":[{"@value":"National Research Institute for Earth Science and Disaster Resilience  Tsukuba Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518172926213","@type":"Researcher","foaf:name":[{"@value":"Takeshi Kimura"}],"jpcoar:affiliationName":[{"@value":"National Research Institute for Earth Science and Disaster Resilience  Tsukuba Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518172926209","@type":"Researcher","foaf:name":[{"@value":"Katsuhiko Shiomi"}],"jpcoar:affiliationName":[{"@value":"National Research Institute for Earth Science and Disaster Resilience  Tsukuba Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2019-04-17","prism:volume":"46","prism:number":"8","prism:startingPage":"4192","prism:endingPage":"4201"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://creativecommons.org/licenses/by-nc-nd/4.0/"],"url":[{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL082448"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2019GL082448"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL082448"}],"createdAt":"2019-04-08","modifiedAt":"2023-08-27","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782015210112","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"19H04626"},{"@type":"JGN","@value":"JP19H04626"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PUBLICLY-19H04626/"}],"notation":[{"@language":"ja","@value":"３次元不均質構造を考慮した南海トラフの浅部超低周波地震の活動様式の網羅的把握"},{"@language":"en","@value":"Characteristics of shallow very low-frequency earthquake activity along the Nankai Trough based on the method incorporating effects of 3D heterogeneous structure model"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256879561344","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H06473"},{"@type":"JGN","@value":"JP16H06473"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-16H06473/"}],"notation":[{"@language":"ja","@value":"海陸機動的観測に基づくスロー地震発生様式の解明"},{"@language":"en","@value":"Study on the Mechanisms Ivolved in the Occurrence of Slow Earthquakes Based on Temporal Inland and Offshore Observations"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202761516800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dynamic deformation of the accretionary prism excites very low frequency earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001338452605568","@type":"Article","resourceType":"学術雑誌論文(journal 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