{"@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/1360021391873188864.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/s41598-023-37474-6"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/s41598-023-37474-6.pdf"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/s41598-023-37474-6"}},{"identifier":{"@type":"PMID","@value":"37429888"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Link between the Nankai underthrust turbidites and shallow slow earthquakes"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Trench sediments such as pelagic clay or terrigenous turbidites have long been invoked to explain the seismogenic behavior of the megathrust fault (i.e., décollement). Recent numerous studies suggest that slow earthquakes may be associated with huge megathrust earthquake; however, controls on the slow earthquake occurrence remain poorly understood. We investigate seismic reflection data along the Nankai Trough subduction zone to understand the correlations between the spatial distribution of the broad turbidites and along-strike variations in shallow slow earthquakes and slip-deficit rates. This report presents a unique map of regional distribution of the three discrete Miocene turbidites that underthrust apparently along the décollement beneath the Nankai accretionary prism. A comparison of distributions of the Nankai underthrust turbidites, shallow slow earthquakes, and slip-deficit rates enables us to infer that the underthrust turbidites may cause primarily low pore-fluid overpressures and high effective vertical stresses across the décollement, leading to potentially inhibiting the slow earthquake occurrence. Our findings provide a new insight into potential role of the underthrust turbidites for shallow slow earthquakes at subduction zone.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380021391873188891","@type":"Researcher","foaf:name":[{"@value":"Jin-Oh Park"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021391873188897","@type":"Researcher","foaf:name":[{"@value":"Ehsan Jamali Hondori"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"20452322"}],"prism:publicationName":[{"@value":"Scientific Reports"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2023-07-10","prism:volume":"13","prism:number":"1","prism:startingPage":"10333"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://creativecommons.org/licenses/by/4.0","https://creativecommons.org/licenses/by/4.0"],"url":[{"@id":"https://www.nature.com/articles/s41598-023-37474-6.pdf"},{"@id":"https://www.nature.com/articles/s41598-023-37474-6"}],"createdAt":"2023-07-10","modifiedAt":"2023-12-16","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Science","dc:title":"Science"},{"@id":"https://cir.nii.ac.jp/all?q=Q","dc:title":"Q"},{"@id":"https://cir.nii.ac.jp/all?q=R","dc:title":"R"},{"@id":"https://cir.nii.ac.jp/all?q=Medicine","dc:title":"Medicine"},{"@id":"https://cir.nii.ac.jp/all?q=Article","dc:title":"Article"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040291932564658176","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"22H00167"},{"@type":"JGN","@value":"JP22H00167"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-22H00167/"}],"notation":[{"@language":"ja","@value":"アウターライズで海洋とマントルを結ぶ大規模流体循環の時空間スケールの解明"},{"@language":"en","@value":"Spatiotemporal scale of large-scale hydrothermal circulation system connecting ocean and mantle at the outer rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1040581301857053696","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23K25964"},{"@type":"JGN","@value":"JP23K25964"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23K25964/"}],"notation":[{"@language":"ja","@value":"沈み込むプレート上部における水の流動の地域による違いとプレート境界への影響の解明"},{"@language":"en","@value":"Fluid flow in the uppermost part of the incoming plate seaward of the trench: Regional variations and influence on processes around the plate interface"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001339107234432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Connecting slow earthquakes to huge earthquakes"},{"@value":"Connecting slow earthquakes to large 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Earthquakes at the Shallow Plate Interface in the Nankai Trough"},{"@language":"ja-Kana","@value":"ナンカイ トラフ ニ オケル センブ スロー ジシンイキ ノ チシツ コウゾウ ト マサツ トクセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417129969536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Simple topographic parameter reveals the along-trench distribution of frictional properties on shallow plate boundary 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