{"@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/1363670320258115712.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/335340a0"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/335340a0"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/335340a0.pdf"}}],"dc:title":[{"@value":"Seismological and structural evolution of strike-slip faults"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320258115712","@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":"1988-09","prism:volume":"335","prism:number":"6188","prism:startingPage":"340","prism:endingPage":"343"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://www.nature.com/articles/335340a0"},{"@id":"http://www.nature.com/articles/335340a0.pdf"}],"createdAt":"2003-06-12","modifiedAt":"2023-05-17","relatedProduct":[{"@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/1360013168732484480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleoearthquake History Along the Southern Segment of the Daliangshan Fault Zone in the Southeastern Tibetan Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283693141019904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of crustal deformation in the northeast–central Japanese island arc: Insights from fault activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292618543890432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The generation of large earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306904388891520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Feature of cascading rupture frequently observed in Northern California"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567184543382272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Correlation between Coulomb stress imparted by the 2011 Tohoku-Oki earthquake and seismicity rate change in Kanto, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092518122496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mainshock and Aftershock Sequence Simulation in Geometrically Complex Fault Zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861705593961728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Earthquake Cycle Deformation Associated With the 2021 <i>M</i><sub><i>W</i></sub> 7.4 Maduo (Eastern Tibet) Earthquake: An Intrablock Rupture Event on a Slow‐Slipping Fault From Sentinel‐1 InSAR and Teleseismic Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303059968","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Numerical Simulation on Faulting: Microscopic Evolution, Macroscopic Interaction and Rupture Process of Earthquakes"},{"@language":"ja","@value":"断層の成長"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240399104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Current issues and a prospective view to the next step for long-term crustal earthquake forecast in Japan"},{"@language":"ja","@value":"内陸地震の長期評価に関する課題と新たな視点"},{"@language":"ja-Kana","@value":"ナイリク ジシン ノ チョウキ ヒョウカ ニ カンスル カダイ ト アラタ ナ シテン"},{"@value":"Current issues and prospective view to the next step for long-term crustal earthquake corecast in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390848647561142016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evolution of Fault Zones and Its Rheology"},{"@language":"ja","@value":"断層帯と断層レオロジーの進化"},{"@language":"ja-Kana","@value":"ダンソウタイ ト ダンソウ レオロジー ノ シンカ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942122898304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamic rupture propagation on geometrically complex fault with along-strike variation of fault maturity : insights from the 2014 Northern Nagano earthquake"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1038/335340a0"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0715-2_references_DOI_U9c4v3EukHK2SHCcnjXxnxkwVKo"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2013.0001_references_DOI_U9c4v3EukHK2SHCcnjXxnxkwVKo"},{"@type":"CROSSREF","@value":"10.1038/s43247-020-00086-3_references_DOI_U9c4v3EukHK2SHCcnjXxnxkwVKo"},{"@type":"CROSSREF","@value":"10.1038/s43017-020-00108-w_references_DOI_U9c4v3EukHK2SHCcnjXxnxkwVKo"},{"@type":"CROSSREF","@value":"10.1029/2018tc005009_references_DOI_U9c4v3EukHK2SHCcnjXxnxkwVKo"},{"@type":"CROSSREF","@value":"10.1111/iar.12179_references_DOI_U9c4v3EukHK2SHCcnjXxnxkwVKo"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.403_references_DOI_U9c4v3EukHK2SHCcnjXxnxkwVKo"},{"@type":"CROSSREF","@value":"10.1038/s43247-025-02138-y_references_DOI_U9c4v3EukHK2SHCcnjXxnxkwVKo"},{"@type":"CROSSREF","@value":"10.1093/gji/ggv001_references_DOI_U9c4v3EukHK2SHCcnjXxnxkwVKo"},{"@type":"CROSSREF","@value":"10.1029/2020jb020865_references_DOI_U9c4v3EukHK2SHCcnjXxnxkwVKo"},{"@type":"CROSSREF","@value":"10.5026/jgeography.129.473_references_DOI_U9c4v3EukHK2SHCcnjXxnxkwVKo"},{"@type":"CROSSREF","@value":"10.1029/2022jb024268_references_DOI_U9c4v3EukHK2SHCcnjXxnxkwVKo"}]}