{"@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/1361137045681667072.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1073/pnas.93.9.3764"}},{"identifier":{"@type":"URI","@value":"https://pnas.org/doi/pdf/10.1073/pnas.93.9.3764"}}],"dc:title":[{"@value":"The repetition of large-earthquake ruptures."}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>This survey of well-documented repeated fault rupture confirms that some faults have exhibited a \"characteristic\" behavior during repeated large earthquakes--that is, the magnitude, distribution, and style of slip on the fault has repeated during two or more consecutive events. In two cases faults exhibit slip functions that vary little from earthquake to earthquake. In one other well-documented case, however, fault lengths contrast markedly for two consecutive ruptures, but the amount of offset at individual sites was similar. Adjacent individual patches, 10 km or more in length, failed singly during one event and in tandem during the other. More complex cases of repetition may also represent the failure of several distinct patches. The faults of the 1992 Landers earthquake provide an instructive example of such complexity. Together, these examples suggest that large earthquakes commonly result from the failure of one or more patches, each characterized by a slip function that is roughly invariant through consecutive earthquake cycles. The persistence of these slip-patches through two or more large earthquakes indicates that some quasi-invariant physical property controls the pattern and magnitude of slip. These data seem incompatible with theoretical models that produce slip distributions that are highly variable in consecutive large events.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004231546202886","@type":"Researcher","foaf:name":[{"@value":"K Sieh"}],"jpcoar:affiliationName":[{"@value":"Seismological Laboratory, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00278424"},{"@type":"EISSN","@value":"10916490"}],"prism:publicationName":[{"@value":"Proceedings of the National Academy of Sciences"}],"dc:publisher":[{"@value":"Proceedings of the National Academy of Sciences"}],"prism:publicationDate":"1996-04-30","prism:volume":"93","prism:number":"9","prism:startingPage":"3764","prism:endingPage":"3771"},"reviewed":"false","url":[{"@id":"https://pnas.org/doi/pdf/10.1073/pnas.93.9.3764"}],"createdAt":"2002-07-26","modifiedAt":"2022-04-13","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004231546203136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coulomb Stress Evolution History as Implication on the Pattern of Strong Earthquakes along the Xianshuihe-Xiaojiang Fault System, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576966733051904","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Application of Vector-Type Super Computer to Understanding Giant Earthquakes and Aftershocks on Subduction Plate Boundaries"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694366743344256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Synchronized gravitational slope deformation and active faulting: A case study on and around the Neodani fault, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205317313408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Consideration on the 2011 off the Pacific Coast of Tohoku Earthquake and the 2004 Sumatra Earthquake"},{"@language":"ja","@value":"東北地方太平洋沖地震・スマトラ島沖地震における連動型地震の考察"}]},{"@id":"https://cir.nii.ac.jp/crid/1390016681646621568","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Advancements in Numa Terrace Investigations for Understanding the History of the Great Kanto Earthquakes"},{"@language":"ja","@value":"関東地震発生履歴解明に向けた房総半島沼段丘群調査の進展"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681490176384","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Earthquake cycles and physical modeling of the process leading up to a large earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714791998694528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Surface rupture and characteristics of a fault associated with the 2011 and 2016 earthquakes in the southern Abukuma Mountains, northeastern Japan, triggered by the Tohoku-Oki earthquake"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1073/pnas.93.9.3764"},{"@type":"CROSSREF","@value":"10.1186/bf03353085_references_DOI_BtR6B7VdVm3L5BuF44UAKUOqXHd"},{"@type":"CROSSREF","@value":"10.1007/s12583-018-0840-2_references_DOI_BtR6B7VdVm3L5BuF44UAKUOqXHd"},{"@type":"CROSSREF","@value":"10.5918/jamstecr.13.17_references_DOI_BtR6B7VdVm3L5BuF44UAKUOqXHd"},{"@type":"CROSSREF","@value":"10.1007/978-3-642-32454-3_6_references_DOI_BtR6B7VdVm3L5BuF44UAKUOqXHd"},{"@type":"CROSSREF","@value":"10.4294/zisin.2023-2s_references_DOI_BtR6B7VdVm3L5BuF44UAKUOqXHd"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1085-8_references_DOI_BtR6B7VdVm3L5BuF44UAKUOqXHd"},{"@type":"CROSSREF","@value":"10.1016/j.geomorph.2020.107214_references_DOI_BtR6B7VdVm3L5BuF44UAKUOqXHd"}]}