{"@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/1360002214351275136.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2017gl073460"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017GL073460"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL073460"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Frictional properties of JFAST core samples and implications for slow earthquakes at the Tohoku subduction zone"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Slow earthquakes occur in the shallow (<20 km deep) part of the Tohoku subduction zone. To understand how frictional properties of the plate boundary fault affect the generation of these slow earthquakes, we conducted friction experiments using borehole samples retrieved from the plate boundary décollement and footwall during Integrated Ocean Drilling Program Expedition 343 (Japan Trench Fast Drilling Project (JFAST)). The plate boundary fault material exhibits a transition from velocity‐strengthening to velocity‐weakening behavior at temperatures between 50 and 150°C, which, in the framework of rate‐and‐state friction laws, is a necessary condition for the generation of slow earthquakes, whereas the footwall sample mainly shows velocity‐strengthening behavior except at temperatures of <50°C. The downdip temperature limit of slow earthquakes in the Japan Trench also lies between 100 and 150°C. Our results suggest that the frictional properties of the plate boundary fault may play a key role in controlling the locations of observed 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  Hiroshima Japan"},{"@value":"Now at Department of Earth Sciences, Faculty of Science Chiba University  Chiba Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380002214351275264","@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/1380002214351275137","@type":"Researcher","foaf:name":[{"@value":"Takehiro Hirose"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Systems Science, Graduate School of Science Hiroshima University  Hiroshima Japan"},{"@value":"Kochi Institute for Core Sample Research JAMSTEC  Nankoku Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380002214351275265","@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/1891428068116324227","@type":"Researcher","foaf:name":[{"@value":"Experimental rock deformation"}]}],"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":"2017-09-09","prism:volume":"44","prism:number":"17","prism:startingPage":"8822","prism:endingPage":"8831"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017GL073460"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL073460"}],"createdAt":"2017-08-29","modifiedAt":"2023-09-09","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=friction","dc:title":"friction"},{"@id":"https://cir.nii.ac.jp/all?q=subduction%20zone","dc:title":"subduction zone"},{"@id":"https://cir.nii.ac.jp/all?q=slow%20earthquakes","dc:title":"slow earthquakes"},{"@id":"https://cir.nii.ac.jp/all?q=Geophysics","dc:title":"Geophysics"},{"@id":"https://cir.nii.ac.jp/all?q=General%20Earth%20and%20Planetary%20Sciences","dc:title":"General Earth and Planetary Sciences"},{"@id":"https://cir.nii.ac.jp/all?q=2011%20Tohoku%20earthquake","dc:title":"2011 Tohoku earthquake"},{"@id":"https://cir.nii.ac.jp/all?q=JFAST","dc:title":"JFAST"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781899081728","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H04064"},{"@type":"JGN","@value":"JP16H04064"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16H04064/"}],"notation":[{"@language":"ja","@value":"熱水摩擦実験に基づくスロー地震発生の物理化学プロセスの解明"},{"@language":"en","@value":"Physicochemical mechanisms underlying frictional responses at slow to fast earthquakes: inferred from hydrothermal friction experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000781959765504","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"17H06455"},{"@type":"JGN","@value":"JP17H06455"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-17H06455/"}],"notation":[{"@language":"ja","@value":"太陽系天体における水-岩石反応"},{"@language":"en","@value":"Water-rock reactionis in Solar System 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