{"@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/1360011144640539776.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/rg021i006p01458"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FRG021i006p01458"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/RG021i006p01458"}}],"dc:title":[{"@value":"Rheology of the lithosphere"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>During the quadrennial term 1979–1982, major advances have been made in our knowledge of the rheology of the oceanic lithosphere by the skillful combination of experimental and theoretical rock mechanics, seismology and marine geophysics in increasingly sophisticated models for the flexure of the oceanic lithosphere at seamounts and island chains, along transform faults, and at subduction zones. The relative simplicity of plate bending geometry, thermal history, and mineralogical and chemical compositions of the oceanic plates in these settings make the geophysical observations very powerful constraints on the in situ rheology of the oceanic lithosphere. In the first part of this paper, I review the laboratory work on materials appropriate to the oceanic lithosphere with emphasis on contributions during the quadrennial period and the need for future work. The important results of flexure models incorporating realistic material properties are then summarized.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380011144640539776","@type":"Researcher","foaf:name":[{"@value":"Stephen H. Kirby"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"87551209"},{"@type":"EISSN","@value":"19449208"}],"prism:publicationName":[{"@value":"Reviews of Geophysics"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1983-07","prism:volume":"21","prism:number":"6","prism:startingPage":"1458","prism:endingPage":"1487"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FRG021i006p01458"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/RG021i006p01458"}],"createdAt":"2008-02-06","modifiedAt":"2025-01-26","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232523299840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rheological structure of northeastern Japan lithosphere based on geophysical observations and rock mechanics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232523450368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Method for correction of differential stress calculations from experiments using the solid salt assembly in a Griggs-type deformation apparatus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232523472768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deformation processes at the down-dip limit of the seismogenic zone: The example of Shimanto accretionary complex"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707150758016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Subduction of the primordial crust into the deep mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302864789814528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Modeling of olivine-spinel phase transformation of germanate olivine (Mg2GeO4) by using the phase-field method"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166015280640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Subduction interface processes recorded by eclogite-facies shear zones (Monviso, W. 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