{"@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/1360584340720259072.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2023jb027762"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2023JB027762"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Transient Creep of Quartz and Granulite at High Temperature Under Wet Conditions"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Transient creep of crustal rocks is important to explain time‐dependent geological processes such as postseismic deformation following a large continental earthquake. While the steady‐state creep flow law parameters of quartz and feldspar, major minerals in the upper and lower crust, are well known, the physical mechanism behind transient creep and the corresponding flow law parameters are poorly understood. We quantify the flow law parameters for both quartz and granulite (mixture of plagioclase and pyroxene) under wet conditions with a nonlinear Burgers model using a Markov chain Monte Carlo (MCMC) method. Modeling results yield an activation energy of 70 ± 20 kJ/mol and a stress exponent of 2.0 ± 0.1 for transient creep of quartz aggregates. For granulite/feldspar, we find activation energies of 280 ± 30 and 220 ± 20 kJ/mol and stress exponents of 1.0 ± 0.2 and 0.9 ± 0.1 under mid (1050–1100°C) and high (1125–1150°C), temperature conditions, respectively. The stress exponents and activation energies of transient creep are consistently smaller than those of steady‐state creep for both quartz and granulite/feldspar. Combined with results for transient creep of olivine that were previously obtained (Masuti & Barbot, 2021, <jats:ext-link xmlns:xlink=\"http://www.w3.org/1999/xlink\" xlink:href=\"https://doi.org/10.1186/s40623-021-01543-9\">https://doi.org/10.1186/s40623-021-01543-9</jats:ext-link>), we suggest that the activation energies and stress exponents of transient creep are smaller than those of steady‐state creep for volumetrically important silicate minerals of the crust and upper mantle. Extrapolation of the estimated flow law parameters of granulite/feldspar to natural conditions suggests that transient creep may dominate during the postseismic period and lasts longer than previously thought.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380584340720259203","@type":"Researcher","foaf:name":[{"@value":"Sagar Masuti"}],"jpcoar:affiliationName":[{"@value":"GFZ German Research Centre for Geosciences  Potsdam Germany"}]},{"@id":"https://cir.nii.ac.jp/crid/1380584340720259201","@type":"Researcher","foaf:name":[{"@value":"Jun Muto"}],"jpcoar:affiliationName":[{"@value":"Tohoku University  Sendai Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380584340720259202","@type":"Researcher","foaf:name":[{"@value":"Erik Rybacki"}],"jpcoar:affiliationName":[{"@value":"GFZ German Research Centre for Geosciences  Potsdam Germany"}]}],"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":"2023-10","prism:volume":"128","prism:number":"10"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://creativecommons.org/licenses/by-nc/4.0/"],"url":[{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2023JB027762"}],"createdAt":"2023-10-06","modifiedAt":"2023-10-26","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=lower%20crust","dc:title":"lower crust"},{"@id":"https://cir.nii.ac.jp/all?q=granulite","dc:title":"granulite"},{"@id":"https://cir.nii.ac.jp/all?q=ddc:550.724","dc:title":"ddc:550.724"},{"@id":"https://cir.nii.ac.jp/all?q=621","dc:title":"621"},{"@id":"https://cir.nii.ac.jp/all?q=rheology","dc:title":"rheology"},{"@id":"https://cir.nii.ac.jp/all?q=quartz","dc:title":"quartz"},{"@id":"https://cir.nii.ac.jp/all?q=feldspar","dc:title":"feldspar"},{"@id":"https://cir.nii.ac.jp/all?q=transient%20creep","dc:title":"transient creep"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040018351903629184","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23K25958"},{"@type":"JGN","@value":"JP23K25958"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23K25958/"}],"notation":[{"@language":"ja","@value":"東北沖地震後の地殻変動・地震活動予測を目指した余効変動モデルの構築"},{"@language":"en","@value":"Postseismic model for predicting crustal deformation and seismicity after the 7Tohoku-oki earthquake"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011142941004544","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rheology of the upper mantle and the mantle wedge: A view from the experimentalists"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143853537408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Transient rheology of the upper mantle beneath central Alaska inferred from the crustal velocity field following the 2002 Denali earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143945711232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Using short‐term postseismic displacements to infer the ambient deformation conditions of the upper mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021396339882496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The effect of water, pressure, and strain on Al/Si order-disorder 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