{"@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/1361699995496731008.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2016gl071932"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016GL071932"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL071932"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2016GL071932"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL071932"}}],"dc:title":[{"@value":"Water vaporization promotes coseismic fluid pressurization and buffers temperature rise"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>We investigated the frictional properties of carbonate‐rich gouge layers at a slip rate of 1.3 m/s, under dry and water‐saturated conditions, while monitoring temperature at different locations on one of the gouge‐host rock interfaces. All experiments showed a peak frictional strength of 0.4–0.7, followed by strong slip weakening to steady state values of 0.1–0.3. Experiments which used a pore fluid with a constant drainage path to the atmosphere showed the development of a temperature plateau beyond 100°C, contemporaneous with the dynamic slip weakening and consistent with thermodynamic considerations of ongoing vaporization of pore water. Upon pore fluid vaporization, the pore pressure increases, while the temperature is buffered endothermically, such that the pore water moves along the liquid‐vapor transition curve in a pressure‐temperature phase diagram. Pore fluid phase transitions of this kind are expected to occur in natural earthquakes at relatively shallow crustal levels, enhancing fluid pressurization while impeding the achievement of high temperatures. Therefore, the operation of vaporization may help explain the low downhole temperature anomalies obtained shortly after large earthquakes.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699995496731010","@type":"Researcher","foaf:name":[{"@value":"Jianye Chen"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Earthquake Dynamics Institute of Geology, China Earthquake Administration  Beijing China"},{"@value":"HPT Laboratory, Department of Earth Sciences Utrecht University  Utrecht Netherlands"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995496731008","@type":"Researcher","foaf:name":[{"@value":"André Niemeijer"}],"jpcoar:affiliationName":[{"@value":"HPT Laboratory, Department of Earth Sciences Utrecht University  Utrecht Netherlands"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995496731011","@type":"Researcher","foaf:name":[{"@value":"Lu Yao"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Earthquake Dynamics Institute of Geology, China Earthquake Administration  Beijing China"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995496731009","@type":"Researcher","foaf:name":[{"@value":"Shengli Ma"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Earthquake Dynamics Institute of Geology, China Earthquake Administration  Beijing China"}]}],"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":"2017-03-06","prism:volume":"44","prism:number":"5","prism:startingPage":"2177","prism:endingPage":"2185"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016GL071932"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL071932"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2016GL071932"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL071932"}],"createdAt":"2017-01-20","modifiedAt":"2023-09-09","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050303932802533248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mechanical Amorphization of Synthetic Fault Gouges During Rotary-Shear Friction Experiments at Subseismic to Seismic Slip Velocities"},{"@value":"Mechanical Amorphization of Synthetic Fault Gouges During Rotary‐Shear Friction Experiments at Subseismic to Seismic Slip Velocities"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092837994240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Influence of Effective Stress and Pore Fluid Pressure on Fault Strength and Slip Localization in Carbonate Slip Zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654737724544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Petrophysical, Geochemical, and Hydrological Evidence for Extensive Fracture‐Mediated Fluid and Heat Transport in the Alpine Fault's Hanging‐Wall Damage Zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865814729797376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Potential Role of Volcanic Glass‐Smectite Mixtures in Slow Earthquakes in Shallow Subduction Zones: Insights From Low‐ to High‐Velocity Friction Experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266985497472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical conductive fluid-rich zones and their influence on the earthquake initiation, growth, and arrest processes : observations from the 2016 Kumamoto earthquake sequence, Kyushu Island, Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2016gl071932"},{"@type":"CROSSREF","@value":"10.1029/2020jb019956_references_DOI_UotcdQE2aVIu6KDdPvPPzEdaufp"},{"@type":"CROSSREF","@value":"10.1029/2020jb019805_references_DOI_UotcdQE2aVIu6KDdPvPPzEdaufp"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01340-w_references_DOI_NJ8GtMrn8TA50W06b6RTmZGKX5C"},{"@type":"CROSSREF","@value":"10.1002/2017gc007202_references_DOI_UotcdQE2aVIu6KDdPvPPzEdaufp"},{"@type":"CROSSREF","@value":"10.1029/2022jb026156_references_DOI_UotcdQE2aVIu6KDdPvPPzEdaufp"}]}