{"@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/1361699994293674624.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2006gl026970"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2006GL026970"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2006GL026970"}}],"dc:title":[{"@value":"Static Coulomb failure function and aftershocks of 1995 Kobe earthquake: A statistical test"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The hypothesis that aftershocks are triggered by a change of the static Coulomb Failure stress is statistically tested for 1995 Kobe (Hyogo‐ken nanbu) Earthquake. We focus on the focal mechanisms of the aftershocks for the first 7 months and investigate whether these mechanisms are consistent with the static CFF triggering hypothesis. Two slip distribution models for the mainshock are tested and both explain focal mechanisms of more than 3/4 of the aftershocks. From a bootstrap statistical test, however, we find that such a high consistency rate between the observation and CFF based prediction is not statistically significant. The static CFF triggering is thus not a statistically strong hypothesis for 1995 Kobe aftershocks.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420564276177176832","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"70335230"},{"@type":"NRID","@value":"1000070335230"},{"@type":"ORCID","@value":"0000-0003-1276-5206"},{"@type":"CINII_AUTHOR_ID","@value":"DA19096275"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA19096275#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA19096275"},{"@type":"NRID","@value":"9000006863031"},{"@type":"NRID","@value":"9000000236962"},{"@type":"NRID","@value":"9000254754501"},{"@type":"NRID","@value":"9000253257228"},{"@type":"NRID","@value":"9000001756587"},{"@type":"NRID","@value":"9000254739184"},{"@type":"NRID","@value":"9000002244174"},{"@type":"NRID","@value":"9000414072563"},{"@type":"NRID","@value":"9000000519603"},{"@type":"NRID","@value":"9000018699073"},{"@type":"NRID","@value":"9000254262074"},{"@type":"NRID","@value":"9000254263190"},{"@type":"NRID","@value":"9000000462215"},{"@type":"NRID","@value":"9000000093565"},{"@type":"NRID","@value":"9000000195796"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0160954"}],"foaf:name":[{"@value":"Mamoru Kato"}],"jpcoar:affiliationName":[{"@value":"Earth Science Group, Graduate School of Human and Environmental Studies Kyoto University  Kyoto Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2006-09","prism:volume":"33","prism:number":"17"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2006GL026970"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2006GL026970"}],"createdAt":"2006-09-11","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001335851923328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Why do aftershocks occur? Relationship between mainshock rupture and aftershock sequence based on highly resolved hypocenter and focal mechanism distributions"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204305619072","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"2011年3月15日静岡県東部地震（Mj6.4）の遅れ誘発過程に関する研究"},{"@language":"en","@value":"Delayed Triggering Process for the Mj6.4 Eastern Shizuoka Earthquake of 15 March 2011"},{"@language":"ja-Kana","@value":"2011ネン 3ガツ 15ニチ シズオカケン トウブ ジシン(Mj6.4)ノ オクレ ユウハツ カテイ ニ カンスル ケンキュウ"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2006gl026970"},{"@type":"OPENAIRE","@value":"doi_dedup___::f91937b73c2dbec3a9748880b39416c9"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0650-2_references_DOI_I1EnYFNDHi9IN9ZuXOMS8C7LvXP"},{"@type":"CROSSREF","@value":"10.4294/zisin.69.99_references_DOI_I1EnYFNDHi9IN9ZuXOMS8C7LvXP"}]}