{"@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/1360283689326464256.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2015gl067569"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2015GL067569"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015GL067569"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2015GL067569"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2015GL067569"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Nucleation of frictional instability caused by fluid pressurization in subducted blueschist"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Pore pressure is an important factor in controlling the slip instability of faults and thus the generation of earthquakes. Particularly slow earthquakes are widespread in subduction zones and usually linked to the occurrence of high pore pressure. Yet the influence of fluid pressure and effective stress on the mechanics of earthquakes is poorly understood. Therefore, we performed shear experiments on blueschist fault rocks, which likely exist at depth in cold and old subduction zones, to investigate the influence of effective stress on frictional behavior. Our results show potentially unstable behavior at temperatures characterizing the seismogenic zone, as well as a transition from stable to unstable behavior with decreasing effective normal stress, which is mechanically equivalent to increasing fluid pressure. This transition is a prerequisite for generating slow earthquakes. Our results imply that high pore pressures are a key factor for nucleating slip leading to both megathrust and slow earthquakes.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420845751137848192","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"20760995"},{"@type":"NRID","@value":"1000020760995"},{"@type":"NRID","@value":"9000347136243"},{"@type":"NRID","@value":"9000350559923"},{"@type":"NRID","@value":"9000350560000"},{"@type":"NRID","@value":"9000258413647"},{"@type":"NRID","@value":"9000410194187"},{"@type":"NRID","@value":"9000350560763"},{"@type":"NRID","@value":"9000350560970"},{"@type":"NRID","@value":"9000347082954"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/msawai"}],"foaf:name":[{"@value":"Michiyo Sawai"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Systems Science, Graduate School of Science Hiroshima University  Higashi‐Hiroshima Japan"},{"@value":"Department of Earth Sciences, Faculty of Science Chiba University  Chiba Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380566392421358851","@type":"Researcher","foaf:name":[{"@value":"André R. Niemeijer"}],"jpcoar:affiliationName":[{"@value":"Department of Earth Sciences Utrecht University  Utrecht Netherlands"}]},{"@id":"https://cir.nii.ac.jp/crid/1380566392421358849","@type":"Researcher","foaf:name":[{"@value":"Oliver Plümper"}],"jpcoar:affiliationName":[{"@value":"Department of Earth Sciences Utrecht University  Utrecht Netherlands"}]},{"@id":"https://cir.nii.ac.jp/crid/1380566392421358850","@type":"Researcher","foaf:name":[{"@value":"Takehiro Hirose"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Systems Science, Graduate School of Science Hiroshima University  Higashi‐Hiroshima Japan"},{"@value":"Kochi Institute for Core Sample Research JAMSTEC  Nankoku Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380566392421358852","@type":"Researcher","foaf:name":[{"@value":"Christopher J. Spiers"}],"jpcoar:affiliationName":[{"@value":"Department of Earth Sciences Utrecht University  Utrecht Netherlands"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1892272492697738500","@type":"Researcher","foaf:name":[{"@value":"Experimental rock deformation"}]},{"@id":"https://cir.nii.ac.jp/crid/1892272492697738501","@type":"Researcher","foaf:name":[{"@value":"Structural geology and EM"}]}],"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":"2016-03-24","prism:volume":"43","prism:number":"6","prism:startingPage":"2543","prism:endingPage":"2551"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2015GL067569"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015GL067569"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2015GL067569"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2015GL067569"}],"createdAt":"2016-03-24","modifiedAt":"2023-09-10","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781835448320","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H06890"},{"@type":"JGN","@value":"JP15H06890"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H06890/"}],"notation":[{"@language":"ja","@value":"スロー地震への間隙水圧の効果"},{"@language":"en","@value":"Pore pressure dependences on frictional behavior of rocks and implications for slow earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256875786752","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H04061"},{"@type":"JGN","@value":"JP16H04061"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16H04061/"}],"notation":[{"@language":"ja","@value":"断層の変形機構遷移を再現した模擬断層実験に基づく新しい断層モデルの構築"},{"@language":"en","@value":"New fault model based on friction experiments across the deformation mechanism transitions"}]},{"@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/1040282257219911424","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"25287135"},{"@type":"JGN","@value":"JP25287135"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-25287135/"}],"notation":[{"@language":"ja","@value":"沈み込み帯の断層レオロジーとスロー地震の発生機構"},{"@language":"en","@value":"Rheology of faults in subduction zones and its implications for the generation of slow earthquakes"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282810792973312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Episodic tremor and slip near the Japan Trench prior to the 2011 Tohoku-Oki earthquake"},{"@value":"Episodic tremor and slip near the Japan Trench prior to the 2011 Tohoku‐Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1050303932805499904","@type":"Article","resourceType":"学術雑誌論文(journal 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