{"@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/1363670318467398528.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1218796"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1218796"}}],"dc:title":[{"@value":"Under the Hood of the Earthquake Machine: Toward Predictive Modeling of the Seismic Cycle"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Earthquake Model Shakedown</jats:title>\n          <jats:p>\n            The Parkfield segment of the San Andreas Fault in California experiences Magnitude 6.0 earthquakes at a surprisingly regular interval—roughly every 22 years. This area is one of the most well studied fault segments in the world, yet computational models often struggle to integrate the wealth of observational data with theoretical predictions.\n            <jats:bold>\n              Barbot\n              <jats:italic>et al.</jats:italic>\n            </jats:bold>\n            (p.\n            <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" page=\"707\" related-article-type=\"in-this-issue\" vol=\"336\" xlink:href=\"10.1126/science.1218796\">707</jats:related-article>\n            ; see the Perspective by\n            <jats:bold>\n              <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" issue=\"6082\" page=\"676\" related-article-type=\"in-this-issue\" vol=\"336\" xlink:href=\"10.1126/science.1220946\">Segall</jats:related-article>\n            </jats:bold>\n            ) constructed a dynamic model of a fault segment which, when integrated with previous observations, reproduces the behavior of the Parkfield segment over the entire earthquake cycle. Because the model is based on realistic fault physics, it not only explains the distribution of small earthquakes but also the recurrence interval of large earthquakes and the amount of geodetic strain accumulated postseismically. It also reveals how smaller earthquakes can influence this region's semiregular earthquake cycle.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670318467398402","@type":"Researcher","foaf:name":[{"@value":"Sylvain Barbot"}],"jpcoar:affiliationName":[{"@value":"Division of Geological and Planetary Sciences, California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318467398401","@type":"Researcher","foaf:name":[{"@value":"Nadia Lapusta"}],"jpcoar:affiliationName":[{"@value":"Division of Geological and Planetary Sciences, California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125, USA."},{"@value":"Division of Engineering and Applied Sciences, California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318467398400","@type":"Researcher","foaf:name":[{"@value":"Jean-Philippe Avouac"}],"jpcoar:affiliationName":[{"@value":"Division of Geological and Planetary Sciences, California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125, USA."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"2012-05-11","prism:volume":"336","prism:number":"6082","prism:startingPage":"707","prism:endingPage":"710"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1218796"}],"createdAt":"2012-05-10","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050003824911645696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Surface creep rate distribution along the Philippine fault, Leyte Island, and possible repeating of Mw ~ 6.5 earthquakes on an isolated locked patch"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848656073912832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Quasi-Dynamic 3D Modeling of the Generation and Afterslip of a Tohoku-oki Earthquake Considering Thermal Pressurization and Frictional Properties of the Shallow Plate Boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567609514752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Complexity in the Earthquake Cycle Increases with the Number of Interacting Patches"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593724550144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Community‐Driven Code Comparisons for Three‐Dimensional Dynamic Modeling of Sequences of Earthquakes and Aseismic Slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869854370617472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Community‐Driven Code Comparisons for Simulations of Fluid‐Induced Aseismic Slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131420852897792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coupled afterslip and transient mantle flow after the 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842049991168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structural control and system-level behavior of the seismic cycle at the Nankai Trough"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.1218796"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1096-5_references_DOI_Yt9sjJ1rHgUz7IDRRU98khbT7gx"},{"@type":"CROSSREF","@value":"10.1007/s00024-018-02089-w_references_DOI_Yt9sjJ1rHgUz7IDRRU98khbT7gx"},{"@type":"CROSSREF","@value":"10.1007/s00024-020-02555-4_references_DOI_Yt9sjJ1rHgUz7IDRRU98khbT7gx"},{"@type":"CROSSREF","@value":"10.1029/2021jb023519_references_DOI_Yt9sjJ1rHgUz7IDRRU98khbT7gx"},{"@type":"CROSSREF","@value":"10.1029/2024jb030601_references_DOI_Yt9sjJ1rHgUz7IDRRU98khbT7gx"},{"@type":"CROSSREF","@value":"10.1126/sciadv.aaw1164_references_DOI_Yt9sjJ1rHgUz7IDRRU98khbT7gx"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-1145-0_references_DOI_Yt9sjJ1rHgUz7IDRRU98khbT7gx"}]}