{"@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/1360292619206503808.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/96jb01926"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F96JB01926"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/96JB01926"}}],"dc:title":[{"@value":"Effects of chemical environment on dislocation creep of quartzite"}],"description":[{"type":"abstract","notation":[{"@value":"The water‐related chemical parameter that affects dislocation creep in quartzite has been determined from variations in sample strength and microstructure with chemical environment in buffered deformation and hydrostatic annealing experiments. Samples were weld‐sealed in double capsules;, , and were buffered using solid oxygen buffers, AgCl or CO2. Black Hills quartzite was deformed at 900°C and 1.5 × 10−5s−1. Two samples were deformed at ∼1700 MPa confining pressure at constant and , with and varying over 8 and 15 orders of magnitude, respectively. Both samples deformed by climb‐accommodated dislocation creep with flow stresses of 300 MPa. Two additional samples were deformed at ∼700 MPa at constant lower than for the 1700‐MPa samples, with varying over 2 orders of magnitude. Both samples faulted with a peak strength of ∼800 MPa. These four experiments suggest no dependence of dislocation creep strength on , or ; instead, a strong dependence of strength on is inferred. Previously deformed samples of Heavitree quartzite were hydrostatically annealed for 4 days at 800°C and 1200 or 500 MPa confining pressure, varying and over 2.5 and 1 order of magnitude, respectively. The microstructures of these samples show increased rates of dislocation climb and grain boundary migration with increasing but no dependence on . These buffered experiments indicate that dislocation creep is affected by alone and suggest that the exponent for the term in the power law creep flow law is >2."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380292619206503809","@type":"Researcher","foaf:name":[{"@value":"Alice D. Post"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292619206503810","@type":"Researcher","foaf:name":[{"@value":"Jan Tullis"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292619206503808","@type":"Researcher","foaf:name":[{"@value":"Richard A. Yund"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1996-10-10","prism:volume":"101","prism:number":"B10","prism:startingPage":"22143","prism:endingPage":"22155"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F96JB01926"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/96JB01926"}],"createdAt":"2004-02-04","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050012570392438528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Water distribution in quartz schists of the Sanbagawa Metamorphic Belt, Japan: infrared spectroscopic mapping and comparison of the calibrations proposed for determining water contents"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216709061888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimates of stress and strain rate in mylonites based on the boundary between the fields of grain‐size sensitive and insensitive creep"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617556400128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rheology of the Fluid Oversaturated Fault Zones at the Brittle‐Plastic Transition"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580229804889600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Water release and homogenization by dynamic recrystallization of quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654736679680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Theoretical derivation of flow laws for quartz dislocation creep: Comparisons with experimental creep data and extrapolation to natural conditions using water fugacity corrections"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892078328960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Strain localization and fabric development in polycrystalline anorthite + melt by water diffusion in an axial deformation experiment"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/96jb01926"},{"@type":"CROSSREF","@value":"10.1029/2011jb008799_references_DOI_CH2IENelKxkRBXIlbfWrWK8Vmc"},{"@type":"CROSSREF","@value":"10.1029/2020jb020804_references_DOI_CH2IENelKxkRBXIlbfWrWK8Vmc"},{"@type":"CROSSREF","@value":"10.5194/se-14-409-2023_references_DOI_CH2IENelKxkRBXIlbfWrWK8Vmc"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0776-2_references_DOI_CH2IENelKxkRBXIlbfWrWK8Vmc"},{"@type":"CROSSREF","@value":"10.1002/2016jb013798_references_DOI_CH2IENelKxkRBXIlbfWrWK8Vmc"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1117-4_references_DOI_CH2IENelKxkRBXIlbfWrWK8Vmc"}]}