{"@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/1361981469021733248.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.273.5279.1202"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.273.5279.1202"}}],"dc:title":[{"@value":"Postseismic Rebound in Fault Step-Overs Caused by Pore Fluid Flow"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Near-field strain induced by large crustal earthquakes results in changes in pore fluid pressure that dissipate with time and produce surface deformation. Synthetic aperture radar (SAR) interferometry revealed several centimeters of postseismic uplift in pull-apart structures and subsidence in a compressive jog along the Landers, California, 1992 earthquake surface rupture, with a relaxation time of 270 ± 45 days. Such a postseismic rebound may be explained by the transition of the Poisson's ratio of the deformed volumes of rock from undrained to drained conditions as pore fluid flow allows pore pressure to return to hydrostatic equilibrium.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981469021733120","@type":"Researcher","foaf:name":[{"@value":"Gilles Peltzer"}],"jpcoar:affiliationName":[{"@value":"G. Peltzer, P. Rosen, F. Rogez, Jet Propulsion Laboratory, 4800 Oak Grove Drive, Pasadena, CA 91109, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469021733248","@type":"Researcher","foaf:name":[{"@value":"Paul Rosen"}],"jpcoar:affiliationName":[{"@value":"G. Peltzer, P. Rosen, F. Rogez, Jet Propulsion Laboratory, 4800 Oak Grove Drive, Pasadena, CA 91109, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469021733249","@type":"Researcher","foaf:name":[{"@value":"Francois Rogez"}],"jpcoar:affiliationName":[{"@value":"G. Peltzer, P. Rosen, F. Rogez, Jet Propulsion Laboratory, 4800 Oak Grove Drive, Pasadena, CA 91109, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469021733250","@type":"Researcher","foaf:name":[{"@value":"Ken Hudnut"}],"jpcoar:affiliationName":[{"@value":"K. Hudnut, U.S. Geological Survey, 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":"1996-08-30","prism:volume":"273","prism:number":"5279","prism:startingPage":"1202","prism:endingPage":"1204"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.273.5279.1202"}],"createdAt":"2006-10-27","modifiedAt":"2024-01-13","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360009142423994240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Decade of Lessons Learned from the 2011 Tohoku‐Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643736032512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Bayesian Inversion for a Stress‐Driven Model of Afterslip and Viscoelastic Relaxation: Method and Application to Postseismic Deformation Following the 2011 <i>M</i><sub><i>W</i></sub> 9.0 Tohoku‐Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206514107648","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Postseismic deformation and the strength of ductile shear zones"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892108505088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamic earthquake sequence simulation with an SBIEM accounting for interseismic poroelastic rebound"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714791998115840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detection of repeating earthquakes and their application in characterizing slow fault slip"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.273.5279.1202"},{"@type":"CROSSREF","@value":"10.1186/bf03353332_references_DOI_Y6cJe4ltQA7voHmsGJ5CuRqEaDy"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0284-z_references_DOI_Y6cJe4ltQA7voHmsGJ5CuRqEaDy"},{"@type":"CROSSREF","@value":"10.1029/2020rg000713_references_DOI_Y6cJe4ltQA7voHmsGJ5CuRqEaDy"},{"@type":"CROSSREF","@value":"10.1029/2020jb021620_references_DOI_Y6cJe4ltQA7voHmsGJ5CuRqEaDy"},{"@type":"CROSSREF","@value":"10.1186/s40623-022-01649-8_references_DOI_Y6cJe4ltQA7voHmsGJ5CuRqEaDy"}]}