{"@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/1360004233287238784.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2010jb008062"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2010JB008062"}},{"identifier":{"@type":"URI","@value":"http://www.agu.org/journals/jb/jb1110/2010JB008062/2010JB008062.pdf"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"On the transient response of serpentine (antigorite) gouge to stepwise changes in slip velocity under high-temperature conditions"}],"description":[{"notation":[{"@value":"[1] Shear-sliding tests were conducted on serpentine (antigorite) gouge to understand the rheology of serpentine-bearing faults. The experiments were carried out using a constant confining pressure (100 MPa), a constant pore water pressure (30 MPa), and a range of temperatures (from room temperature to 600°C). The transient response in frictional behavior following stepwise changes in the slip velocity were documented at each temperature. Slip rates varied between 0.0115 and 11.5 μm/s. Both the general level of frictional strength and the transient responses changed drastically at around 450°C. As the temperature increased from 400°C to 450°C, the strength of antigorite rose sharply. The transient response also indicated a change in the mode of deformation from flow-type behavior at temperatures below 400°C to frictional behavior (stick-slip) at temperatures above 450°C–500°C. Although only a limited volume of serpentine was involved in the dehydration reaction, X-ray diffraction analyses and scanning electron microscopy observations showed that forsterite had nucleated in the experimental products at the higher temperatures that were associated with frictional behavior. Submicron-sized, streaky forsterite masses in shear-localized zones may be evidence of shear-induced dehydration that caused strengthening and embrittlement of the gouge. Although antigorite rheology is complicated, the subsequent change in friction coefficient per order-of-magnitude change in sliding velocity increased with both increasing temperature and decreasing velocity, implying that a possible flow mechanism of intragranular deformation became activated."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420282801197341696","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40470033"},{"@type":"NRID","@value":"1000040470033"},{"@type":"NRID","@value":"9000001998534"},{"@type":"NRID","@value":"9000004618940"},{"@type":"NRID","@value":"9000311498092"},{"@type":"NRID","@value":"9000399224099"},{"@type":"NRID","@value":"9000254263303"},{"@type":"NRID","@value":"9000267810247"},{"@type":"NRID","@value":"9000257916693"},{"@type":"NRID","@value":"9000346936623"},{"@type":"NRID","@value":"9000014233460"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0138382"}],"foaf:name":[{"@value":"Miki Takahashi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233287239169","@type":"Researcher","foaf:name":[{"@value":"Shin-Ichi Uehara"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233287238664","@type":"Researcher","foaf:name":[{"@value":"Kazuo Mizoguchi"}]},{"@id":"https://cir.nii.ac.jp/crid/1420001326231343488","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40211966"},{"@type":"NRID","@value":"1000040211966"},{"@type":"ORCID","@value":"0000-0001-5269-9675"},{"@type":"NRID","@value":"9000283245948"},{"@type":"NRID","@value":"9000267810250"},{"@type":"NRID","@value":"9000408475228"},{"@type":"NRID","@value":"9000001748486"},{"@type":"NRID","@value":"9000398261217"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/rheology"}],"foaf:name":[{"@value":"Ichiko Shimizu"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233287239175","@type":"Researcher","foaf:name":[{"@value":"Keishi Okazaki"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233287238786","@type":"Researcher","foaf:name":[{"@value":"Koji Masuda"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2011-10-18","prism:volume":"116","prism:number":"B10","prism:startingPage":"B10405"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://doi.wiley.com/10.1002/tdm_license_1.1"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2010JB008062"},{"@id":"http://www.agu.org/journals/jb/jb1110/2010JB008062/2010JB008062.pdf"}],"createdAt":"2011-08-05","modifiedAt":"2021-07-22","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=450","dc:title":"450"},{"@id":"https://cir.nii.ac.jp/all?q=669","dc:title":"669"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782062633344","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"21107004"},{"@type":"JGN","@value":"JP21107004"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-21107004/"}],"notation":[{"@language":"ja","@value":"巨大地震断層の力学的・水理学的特性の解明"},{"@language":"en","@value":"Mechanical and hydrological properties of mega-earthquake thrusts"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257039589504","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"21109005"},{"@type":"JGN","@value":"JP21109005"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-21109005/"}],"notation":[{"@language":"ja","@value":"地殻流体の形態と物性"},{"@language":"en","@value":"Microstructure and Physical Properties of intergranular Geofluids"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257086608640","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"22340148"},{"@type":"JGN","@value":"JP22340148"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-22340148/"}],"notation":[{"@language":"ja","@value":"高温高圧変形実験による蛇紋岩のレオロジー解明"},{"@language":"en","@value":"Rheology of serpentinites clarified by high-PT deformation 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