{"@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/1362262943315927040.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/nature05275"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/nature05275.pdf"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/nature05275"}}],"dc:title":[{"@value":"Predicting the endpoints of earthquake ruptures"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262943315927040","@type":"Researcher","foaf:name":[{"@value":"Steven G. Wesnousky"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00280836"},{"@type":"EISSN","@value":"14764687"}],"prism:publicationName":[{"@value":"Nature"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2006-11","prism:volume":"444","prism:number":"7117","prism:startingPage":"358","prism:endingPage":"360"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://www.nature.com/articles/nature05275.pdf"},{"@id":"http://www.nature.com/articles/nature05275"}],"createdAt":"2006-11-16","modifiedAt":"2024-02-08","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050570796194565888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stress relaxation arrested the mainshock rupture of the 2016 Central Tottori earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142616389120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Conjugate faulting and structural complexity on the young fault system associated with the 2000 Tottori earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707500198656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tectonic geomorphology and paleoseismology of the Surigao segment of the Philippine fault in northeastern Mindanao Island, Philippines"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617435485824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Curvature, a mechanical link between the geometrical complexities of a fault: application to bends, kinks and rough faults"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306905605997440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geomorphologic mapping and analysis of fault activities along the northern margin of the Yanfan Basin, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580229814381696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamic simulations of coseismic slickenlines on non-planar and rough faults"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580230588188288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial change in differential stress magnitudes around the source fault before intraplate earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657453657216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Physics of Earthquake Rupture Propagation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848661058548352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Statistical properties of Olami-Feder-Christensen model on Barabasi-Albert scale-free network"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567354121216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Relationship Between Seismic and Aseismic Slip on the Philippine Fault on Leyte Island: Bayesian Modeling of Fault Slip and Geothermal Subsidence"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869856031123584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Nonplanar 3D fault geometry controls the spatiotemporal distributions of slip and uplift: evidence from the Mw 7.5 2024 Noto Peninsula, Japan, Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206239553152","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Surface rupture and slip associated with the 2014 Nagano-ken Hokubu earthquake（Mw6.2）"},{"@language":"ja","@value":"2014年長野県北部の地震（Mw6.2）に伴う地表地震断層の分布と変位量"},{"@language":"ja-Kana","@value":"2014ネン ナガノケン ホクブ ノ ジシン(Mw6.2)ニ トモナウ チヒョウ ジシン ダンソウ ノ ブンプ ト ヘンイリョウ"},{"@value":"Surface rupture and slip associated with the 2014 Nagano‐ken Hokubu earthquake (Mw 6.2)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390300302109572864","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Long-term forecast and occurrence probability based on past multi-segment megaquakes on the ISTL active fault zone"},{"@language":"ja","@value":"糸魚川-静岡構造線断層帯における連動型巨大地震の発生可能性評価"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238103755776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fault Distribution, Segmentation and Earthquake Generation Potential of the Philippine Fault in Eastern Mindanao, Philippines"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433316889479296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Slip-partitioned surface ruptures for the Mw 7.0 16 April 2016 Kumamoto, Japan, earthquake"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1038/nature05275"},{"@type":"CROSSREF","@value":"10.20965/jdr.2015.p0074_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"},{"@type":"CROSSREF","@value":"10.1038/s43247-020-00086-3_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2018.04.013_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"},{"@type":"CROSSREF","@value":"10.1093/gji/ggaa308_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"},{"@type":"CROSSREF","@value":"10.1016/j.geomorph.2024.109568_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"},{"@type":"CROSSREF","@value":"10.4116/jaqua.63.2219_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"},{"@type":"CROSSREF","@value":"10.1093/gji/ggac501_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"},{"@type":"CROSSREF","@value":"10.1093/gji/ggac521_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0560-8_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"},{"@type":"CROSSREF","@value":"10.1140/epjb/e2017-80295-0_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"},{"@type":"CROSSREF","@value":"10.1029/2020jb020052_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"},{"@type":"CROSSREF","@value":"10.1038/s43247-021-00231-6_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"},{"@type":"CROSSREF","@value":"10.1186/s40623-025-02187-9_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2017.02.001_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2016.0048_references_DOI_7BXv8WWwIR60QJJTTKWhOErcb4z"}]}