{"@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/1363670318939520512.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2007gl031169"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2007GL031169"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007GL031169"}}],"dc:title":[{"@value":"Three‐dimensional distributions of <i>S</i> wave reflectors in the source region of the 2000 Western Tottori Earthquake"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We conducted a reflection analysis of the aftershock waveforms in the source region of the 2000 Western Tottori Earthquake. We obtained three‐dimensional distributions of <jats:italic>S</jats:italic> wave reflectors in the source region by using ∼9000 waveform traces. In the cross‐section projected along the mainshock fault plane, we found three major reflection zones at depths of 15–25 km, 30–40 km and 50–60 km. The first and second are thought to correspond to the Conrad and the Moho discontinuities. The depth of these reflective zones seems to change along the fault direction. Also, cross‐sections perpendicular to the fault plane show that the strengths of the reflected waves are different between the two sides of the fault plane. This result suggests that the mainshock fault plane is located at the boundary of medium properties and its near‐vertical downward extension in the lower crust.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670318939520512","@type":"Researcher","foaf:name":[{"@value":"Issei Doi"}],"jpcoar:affiliationName":[{"@value":"Disaster Prevention Research Institute Kyoto University  Uji Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318939520513","@type":"Researcher","foaf:name":[{"@value":"Kin'ya Nishigami"}],"jpcoar:affiliationName":[{"@value":"Disaster Prevention Research Institute Kyoto University  Uji 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":"2007-10","prism:volume":"34","prism:number":"20","prism:startingPage":"L20312"},"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%2F2007GL031169"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007GL031169"}],"createdAt":"2007-10-25","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001335835719808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-dimensional distribution of S wave reflectors in the northern Kinki district, southwestern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360301469292674688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Upward Earthquake Swarm Migration in the Northeastern Noto Peninsula, Japan, Initiated From a Deep Ring‐Shaped Cluster: Possibility of Fluid Leakage From a Hidden Magma System"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204302999552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Receiver Function Analyses for Estimating Seismic Velocity Discontinuity Structure"},{"@language":"ja","@value":"レシーバ関数解析による地震波速度不連続構造"},{"@language":"ja-Kana","@value":"レシーバ カンスウ カイセキ ニ ヨル ジシンハ ソクド フレンゾク コウゾウ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417112306048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The relationship between S-wave reflectors and deep low-frequency earthquakes in the northern Kinki district, southwestern Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2007gl031169"},{"@type":"OPENAIRE","@value":"doi_dedup___::6323e911e03990c5114668473391ac22"},{"@type":"CROSSREF","@value":"10.1029/2022jb026047_references_DOI_ZmFhbqdbWikKzZKqocnqtURZV11"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.199_references_DOI_KKQqAxwuVRai96gE4SWV21q3aIX"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0468-3_references_DOI_KKQqAxwuVRai96gE4SWV21q3aIX"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0921-6_references_DOI_KKQqAxwuVRai96gE4SWV21q3aIX"}]}