{"@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/1360286993149768192.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2019gl084666"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL084666"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2019GL084666"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL084666"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Migrations and Clusters of Shallow Very Low Frequency Earthquakes in the Regions Surrounding Shear Stress Accumulation Peaks Along the Nankai Trough"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The spatiotemporal characteristics of shallow slow earthquake activity are linked to the tectonic environments of shallow plate boundaries. In this work, the spatiotemporal variations of shallow very low frequency earthquake (SVLFE) activity along the Nankai Trough were investigated using a cross‐correlation analysis. The SVLFEs migrated or spread eastward along the strike direction of the trench during large SVLFE episodes. Migrations and clusters of SVLFEs suggest the occurrence of shallow slow slip events. The observed lateral variations in SVLFE activity patterns reflect the heterogeneous distributions of effective strengths at the shallow plate boundary along the Nankai Trough. Migrations and clusters of SVLFEs tended to be concentrated in the regions surrounding the stress accumulation peaks on the Philippine Sea Plate boundary. The stress accumulated in the transitional regions between high‐strength and low‐strength zones can be released by shallow slow earthquakes.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380286993149768448","@type":"Researcher","foaf:name":[{"@value":"Shunsuke Takemura"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute The University of Tokyo  Bunkyo‐ku Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380286993149768320","@type":"Researcher","foaf:name":[{"@value":"Akemi Noda"}],"jpcoar:affiliationName":[{"@value":"Earthquake and Tsunami Research Division National Research Institute for Earth Science and Disaster Resilience  Tsukuba Ibaraki Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801189987072","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"70808071"},{"@type":"NRID","@value":"1000070808071"},{"@type":"NRID","@value":"9000414332559"},{"@type":"NRID","@value":"9000415327093"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/kubotatsu"}],"foaf:name":[{"@value":"Tatsuya Kubota"}],"jpcoar:affiliationName":[{"@value":"Network Center for Earthquake, Tsunami and Volcano National Research Institute for Earth Science and Disaster Resilience  Tsukuba Ibaraki Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380286993149768449","@type":"Researcher","foaf:name":[{"@value":"Youichi Asano"}],"jpcoar:affiliationName":[{"@value":"Network Center for Earthquake, Tsunami and Volcano National Research Institute for Earth Science and Disaster Resilience  Tsukuba Ibaraki Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380286993149768322","@type":"Researcher","foaf:name":[{"@value":"Takanori Matsuzawa"}],"jpcoar:affiliationName":[{"@value":"Network Center for Earthquake, Tsunami and Volcano National Research Institute for Earth Science and Disaster Resilience  Tsukuba Ibaraki Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380286993149768193","@type":"Researcher","foaf:name":[{"@value":"Katsuhiko Shiomi"}],"jpcoar:affiliationName":[{"@value":"Network Center for Earthquake, Tsunami and Volcano National Research Institute for Earth Science and Disaster Resilience  Tsukuba Ibaraki 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":"2019-11-07","prism:volume":"46","prism:number":"21","prism:startingPage":"11830","prism:endingPage":"11840"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL084666"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2019GL084666"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL084666"}],"createdAt":"2019-10-16","modifiedAt":"2023-08-30","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"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256888039296","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16K05536"},{"@type":"JGN","@value":"JP16K05536"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16K05536/"}],"notation":[{"@language":"ja","@value":"継続時間を考慮した西南日本のスロースリップイベント観測解析手法の開発"},{"@language":"en","@value":"Development on analysis 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