{"@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/1390282681522583552.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2465/jmps.150421"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/jmps/110/6/110_150421/_pdf"}},{"identifier":{"@type":"NAID","@value":"130005115719"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@language":"en","@value":"Effect of temperature on the frictional behavior of smectite and illite"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"We performed high–temperature friction experiments to investigate the effect of temperature on the frictional behavior of smectite and illite. Friction coefficients (<i>μ</i>) of these clay minerals increase with increasing temperature as a result of dehydration of absorbed and interstitial water. At a constant normal stress of 60 MPa, <i>μ</i> of Ca–smectite gouge increases from 0.27 at room temperature to 0.67 at 200 °C, and <i>μ</i> of illite gouge increase from 0.53 at room temperature to 0.68 at 200 °C. Velocity dependence of steady–state friction for smectite and illite gouges changes with temperature so that the transition from velocity–strengthening to velocity–weakening behavior occurs at 150 °C at a normal stress of 60 MPa. Temperature at which this change takes place corresponds to the temperature at the updip limit of the seismogenic zone along subducting plates. Thus, the effect of temperature on the frictional behavior of these clay minerals possibly play an important role in controlling the updip limit of subduction thrust earthquakes."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410282681522583553","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000312721911"}],"foaf:name":[{"@language":"en","@value":"KUBO Tatsuro"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Earth and Planetary Systems Science, Hiroshima University"}]},{"@id":"https://cir.nii.ac.jp/crid/1420001326217299712","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"10448235"},{"@type":"NRID","@value":"1000010448235"},{"@type":"NRID","@value":"9000018783019"},{"@type":"NRID","@value":"9000267805704"},{"@type":"NRID","@value":"9000016926788"},{"@type":"NRID","@value":"9000267790470"},{"@type":"NRID","@value":"9000361693190"},{"@type":"NRID","@value":"9000411958562"},{"@type":"NRID","@value":"9000259833927"},{"@type":"NRID","@value":"9000267798470"},{"@type":"NRID","@value":"9000283729299"},{"@type":"NRID","@value":"9000018228478"},{"@type":"NRID","@value":"9000312721912"},{"@type":"NRID","@value":"9000402492014"},{"@type":"NRID","@value":"9000347136377"},{"@type":"NRID","@value":"9000345221359"},{"@type":"NRID","@value":"9000004618776"},{"@type":"NRID","@value":"9000347191414"},{"@type":"NRID","@value":"9000297496715"},{"@type":"NRID","@value":"9000327448711"},{"@type":"NRID","@value":"9000409996495"},{"@type":"NRID","@value":"9000398794454"},{"@type":"NRID","@value":"9000267798620"},{"@type":"NRID","@value":"9000331096688"},{"@type":"NRID","@value":"9000376926081"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0154534"}],"foaf:name":[{"@language":"en","@value":"KATAYAMA Ikuo"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Earth and Planetary Systems Science, Hiroshima University"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13456296"},{"@type":"LISSN","@value":"13456296"},{"@type":"EISSN","@value":"13493825"}],"prism:publicationName":[{"@language":"en","@value":"Journal of Mineralogical and Petrological Sciences"},{"@language":"en","@value":"Journal of Mineralogical and Petrological Sciences"}],"dc:publisher":[{"@language":"en","@value":"Japan Association of Mineralogical Sciences"},{"@language":"ja","@value":"一般社団法人　日本鉱物科学会"}],"prism:publicationDate":"2015","prism:volume":"110","prism:number":"6","prism:startingPage":"293","prism:endingPage":"299"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"https://www.jstage.jst.go.jp/article/jmps/110/6/110_150421/_pdf"}],"availableAt":"2015","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Frictional%20properties","dc:title":"Frictional properties"},{"@id":"https://cir.nii.ac.jp/all?q=Velocity%20dependence","dc:title":"Velocity dependence"},{"@id":"https://cir.nii.ac.jp/all?q=Smectite%E2%80%93illite%20transition","dc:title":"Smectite–illite transition"},{"@id":"https://cir.nii.ac.jp/all?q=Updip%20limit%20of%20the%20seismogenic%20zone","dc:title":"Updip limit of the seismogenic zone"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781825261440","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H02147"},{"@type":"JGN","@value":"JP15H02147"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H02147/"}],"notation":[{"@language":"ja","@value":"粘土鉱物の摩擦特性に対する湿度・水溶液の効果"},{"@language":"en","@value":"Effect of humidity and fluid on frictional property of clay minerals"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011145474388864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Frictional and hydrologic properties of clay‐rich fault gouge"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021390740597504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A small amount of water reduces the friction of the preferentially oriented montmorillonite 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Friction of the Smectite Clay Montmorillonite"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519591753472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Influence of subduction zone conditions and gouge composition on frictional slip stability of megathrust faults"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694368033642240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"First‐principles Investigation of Frictional Characteristics of Brucite: An Application to Its Macroscopic Frictional Characteristics"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994374038912","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Shearing of saturated clays in rock joints at high confining pressures"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994784210560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Correlation between velocity dependence of friction and strain localization in large displacement experiments on feldspar, muscovite and biotite gouge"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699996149732608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modelling of short-interval silent slip events in deeper subduction interfaces considering the frictional properties at the unstable-stable transition regime"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981471029956480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Updip limit of the seismogenic zone beneath the accretionary prism of southwest Japan: An effect of diagenetic to low-grade metamorphic processes and increasing effective stress"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981471073114624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Constraints on the stress state of the San Andreas Fault with analysis based on core and cuttings from San Andreas Fault Observatory at Depth (SAFOD) drilling phases 1 and 2"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981471310349184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Depth of seismic coupling along subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943463419264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effect of hydration state on the frictional properties of montmorillonite‐based fault gouge"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894190055424","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The seismogenic zone of subduction thrust faults"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895262711168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the mechanical role of smectite in subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895428232832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sliding behavior and deformation textures of heated illite gouge"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370528551040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Comparison of smectite- and illite-rich gouge frictional properties: application to the updip limit of the seismogenic zone along subduction megathrusts"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370704764416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modeling of rock friction: 1. 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