{"@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/1361975843008977280.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2018jb017205"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018JB017205"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB017205"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018JB017205"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB017205"}},{"identifier":{"@type":"DOI","@value":"10.17605/osf.io/h8ue7"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Frictional Properties of Simulated Chlorite Gouge at Hydrothermal Conditions: Implications for Subduction Megathrusts"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Chlorite is abundant at hypocentral depths in subduction zones and is likely to play a key role in controlling megathrust slow slip and catastrophic rupture. However, no data exist on the frictional properties of chlorite(‐rich) fault rocks under the hydrothermal conditions relevant for the subduction seismogenic zone. We report results from experiments conducted under such conditions, using chlorite powders prepared from single crystal clinochlore (Mg‐chlorite), as well as limited experiments using a stack of single crystal sheets. Shear experiments were carried out at effective normal stresses (<jats:italic>σ</jats:italic><jats:sub><jats:italic>n</jats:italic></jats:sub>) of 100 to 400 MPa, pore fluid pressures (<jats:italic>P</jats:italic><jats:sub><jats:italic>f</jats:italic></jats:sub>) of 50 to 220 MPa, and at temperatures (<jats:italic>T</jats:italic>) of 22 to 600 °C, using stepped displacement rates (<jats:italic>v</jats:italic>) from 0.3 to 100 μm/s. The gouges are characterized by a coefficient of friction (<jats:italic>μ</jats:italic>) of 0.2–0.3 at <jats:italic>T</jats:italic> ≤ 400 °C and 0.3–0.4 at 500–600 °C, while (<jats:italic>a‐b</jats:italic>) values showed positive values for nearly all conditions tested, except at 300 °C. Microstructures of gouges sheared at <jats:italic>T</jats:italic> ≤ 300 °C show evidence for widespread comminution, compared with a lower porosity at 600 °C. Experiments using a stack of single crystal sheets showed <jats:italic>μ</jats:italic> ≤ 0.008 at low displacements (<3 mm) followed by hardening, while microstructures are suggestive of slip along (001), folding and tear of cleavage planes, and gouge production. Our results have important implications for the mechanisms controlling megathrust fault slip under greenschist facies conditions in a subduction zone and shed new light on the strain accommodation mechanisms within sheared gouges versus single crystals composed of phyllosilicates.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381975843008977536","@type":"Researcher","foaf:name":[{"@value":"Ayumi S. Okamoto"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Sciences, Graduate School of Science University of Tokyo  Tokyo Japan"},{"@value":"High Pressure and Temperature Laboratory Utrecht University  Utrecht Netherlands"}]},{"@id":"https://cir.nii.ac.jp/crid/1381975843008977409","@type":"Researcher","foaf:name":[{"@value":"Berend A. Verberne"}],"jpcoar:affiliationName":[{"@value":"Geological Survey of Japan National Institute of Advanced Industrial Science and Technology  Tsukuba Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381975843008977410","@type":"Researcher","foaf:name":[{"@value":"André R. Niemeijer"}],"jpcoar:affiliationName":[{"@value":"High Pressure and Temperature Laboratory Utrecht University  Utrecht Netherlands"}]},{"@id":"https://cir.nii.ac.jp/crid/1381975843008977408","@type":"Researcher","foaf:name":[{"@value":"Miki Takahashi"}],"jpcoar:affiliationName":[{"@value":"Geological Survey of Japan National Institute of Advanced Industrial Science and Technology  Tsukuba Japan"}]},{"@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"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Sciences, Graduate School of Science University of Tokyo  Tokyo Japan"},{"@value":"Division of Earth and Planetary Sciences, Graduate School of Science Kyoto University  Kyoto Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381975843008977281","@type":"Researcher","foaf:name":[{"@value":"Tadamasa Ueda"}],"jpcoar:affiliationName":[{"@value":"Division of Earth and Planetary Sciences, Graduate School of Science Kyoto University  Kyoto Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381975843008977537","@type":"Researcher","foaf:name":[{"@value":"Christopher J. Spiers"}],"jpcoar:affiliationName":[{"@value":"High Pressure and Temperature Laboratory Utrecht University  Utrecht Netherlands"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1892272492942080388","@type":"Researcher","foaf:name":[{"@value":"Experimental rock deformation"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"21699313"},{"@type":"EISSN","@value":"21699356"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2019-05","prism:volume":"124","prism:number":"5","prism:startingPage":"4545","prism:endingPage":"4565"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018JB017205"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB017205"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018JB017205"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB017205"}],"createdAt":"2019-04-25","modifiedAt":"2023-09-07","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=megathrust","dc:title":"megathrust"},{"@id":"https://cir.nii.ac.jp/all?q=Geophysics","dc:title":"Geophysics"},{"@id":"https://cir.nii.ac.jp/all?q=chlorite","dc:title":"chlorite"},{"@id":"https://cir.nii.ac.jp/all?q=Geochemistry%20and%20Petrology","dc:title":"Geochemistry and Petrology"},{"@id":"https://cir.nii.ac.jp/all?q=Space%20and%20Planetary%20Science","dc:title":"Space and Planetary Science"},{"@id":"https://cir.nii.ac.jp/all?q=earthquake","dc:title":"earthquake"},{"@id":"https://cir.nii.ac.jp/all?q=Taverne","dc:title":"Taverne"},{"@id":"https://cir.nii.ac.jp/all?q=Earth%20and%20Planetary%20Sciences%20(miscellaneous)","dc:title":"Earth and Planetary Sciences (miscellaneous)"},{"@id":"https://cir.nii.ac.jp/all?q=subduction","dc:title":"subduction"},{"@id":"https://cir.nii.ac.jp/all?q=phyllosilicate","dc:title":"phyllosilicate"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782022151552","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"19K14823"},{"@type":"JGN","@value":"JP19K14823"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-19K14823/"}],"notation":[{"@language":"en","@value":"Material-physical processes controlling fault-slip at the depth limits of the seismogenic zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257255926784","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26109005"},{"@type":"JGN","@value":"JP26109005"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-26109005/"}],"notation":[{"@language":"ja","@value":"岩石変形実験による地殻の力学物性の解明：流体の影響"},{"@language":"en","@value":"Exploring the mechanical properties of crustal materials through rock deformation experiments: Influence of geofluids"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202746187904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional seismic velocity structure and configuration of the Philippine Sea slab in southwestern Japan estimated by double-difference tomography"}]},{"@id":"https://cir.nii.ac.jp/crid/1050306506454155648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Alteration and dehydration of subducting oceanic crust within subduction zones : implications for decollement step-down and plate-boundary seismogenesis"},{"@value":"Alteration and dehydration of subducting oceanic crust within subduction zones : implications for décollement step-down and plate-boundary seismogenesis"}]},{"@id":"https://cir.nii.ac.jp/crid/1050574290291764480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Hydrous oceanic crust hosts megathrust creep at low shear stresses"},{"@value":"Hydrous oceanic crust hosts megathrust creep at low shear zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216708835840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stuck in the mud? 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