{"@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/1363670320654879488.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2000gc000036"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2000GC000036"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2000GC000036"}}],"dc:title":[{"@value":"Self‐consistent generation of tectonic plates in time‐dependent, three‐dimensional mantle convection simulations"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Presented here are self‐consistent, three‐dimensional simulations of mantle convection, some of which display an approximation of plate tectonic behavior that is continuous in space and time. Plate behavior arises through a reasonable material description of silicate deformation, with a simple yield stress being sufficient to give first‐order plate‐like behavior; however, the required yield strength or fault frictional coefficient is much less than experimentally determined values. Toroidal:poloidal ratios are within geologically observed limits. The sensitivity of the system to yield strength and the form of strength envelope is systematically investigated. Optimum plate character is obtained in a narrow range of yield strength, below which diffuse boundaries, and above which episodic behavior, and eventually a rigid lid, are observed. Models with mobile lids develop very long wavelength horizontal structure, the longest wavelength possible in the domain. Two‐dimensional models display much greater time dependence than three‐dimensional models.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320654879488","@type":"Researcher","foaf:name":[{"@value":"Paul J. Tackley"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Space Sciences University of California  Los Angeles USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"15252027"},{"@type":"EISSN","@value":"15252027"}],"prism:publicationName":[{"@value":"Geochemistry, Geophysics, Geosystems"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2000-08","prism:volume":"1","prism:number":"8","prism:startingPage":"2000GC000036"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2000GC000036"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2000GC000036"}],"createdAt":"2004-02-04","modifiedAt":"2023-10-29","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050012570393434752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three‐dimensional numerical modeling of temperature and mantle flow fields associated with subduction of the Philippine Sea plate, southwest Japan"},{"@value":"Three-dimensional numerical modeling of temperature and mantle flow fields associated with subduction of the Philippine Sea plate, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229803591168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Influence of plate tectonic mode on the coupled thermochemical evolution of Earth's mantle and core"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179755238528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Water circulation and global mantle dynamics: Insight from numerical modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092436780544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heat‐Blanketed Convection and its Implications for the Continental Lithosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092694097280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimation of Secular Change in the Size of Continents for Understanding Early Crustal Development"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848656092233344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A linear stability analysis on the onset of thermal convection of a fluid with strongly temperature-dependent viscosity in a spherical shell"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892145971840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Analysis of plate spin motion and its implications for strength of plate boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266844293248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of the rheological structure of Mars"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2000gc000036"},{"@type":"CROSSREF","@value":"10.1002/2015gc005996_references_DOI_Tow0lM0UfczDIsPKZeGvnCRduAv"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0593-z_references_DOI_Tow0lM0UfczDIsPKZeGvnCRduAv"},{"@type":"CROSSREF","@value":"10.1002/2016jb012912_references_DOI_Tow0lM0UfczDIsPKZeGvnCRduAv"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0405-5_references_DOI_Tow0lM0UfczDIsPKZeGvnCRduAv"},{"@type":"CROSSREF","@value":"10.1029/2020jb020695_references_DOI_Tow0lM0UfczDIsPKZeGvnCRduAv"},{"@type":"CROSSREF","@value":"10.1002/2014gc005701_references_DOI_Tow0lM0UfczDIsPKZeGvnCRduAv"},{"@type":"CROSSREF","@value":"10.3389/feart.2020.541094_references_DOI_Tow0lM0UfczDIsPKZeGvnCRduAv"},{"@type":"CROSSREF","@value":"10.1007/s00162-011-0250-x_references_DOI_Tow0lM0UfczDIsPKZeGvnCRduAv"}]}