{"@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/1363670320202003584.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/96gl02765"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F96GL02765"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/96GL02765"}}],"dc:title":[{"@value":"Seismic evidence for stretched continental crust in the Japan Sea"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The Japan Sea is a major marginal sea in the western Pacific comprised of basins and bathymetric highs. Technically, these features were created by multiple‐rifting and spreading processes, as exemplified in the creation of the Japan Basin and Yamato Basin. However, there are smaller scale features for which seismic crustal models have been inadequate to infer or verify their origin and evolution. Recent advances in marine seismological surveys enable us to obtain heterogeneous seismic crustal structures in sufficient detail to characterize these features. In September of 1992, a seismic experiment was conducted to obtain the detailed seismic crustal structure in the southwestern part of the Japan Sea, including the basin and bank areas. Seventeen ocean bottom seismometers (OBSs) were deployed on two lines. Explosives and airguns were fired as controlled seismic sources. The model of the crust obtained in the northern Tsushima Basin is about 13 km thick including a 1.5‐km‐thick sedimentary layer. Beneath the bank area the crust is 22 km thick and the upper crust is relatively homogeneous with a <jats:italic>P</jats:italic>‐wave velocity of about 6 km/s. The bank is interpreted to be a stretched continental crust fragment.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320202003588","@type":"Researcher","foaf:name":[{"@value":"Eiji Kurashimo"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320202003586","@type":"Researcher","foaf:name":[{"@value":"Masanao Shinohara"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320202003584","@type":"Researcher","foaf:name":[{"@value":"Kiyoshi Suyehiro"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320202003585","@type":"Researcher","foaf:name":[{"@value":"Junzo Kasahara"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320202003587","@type":"Researcher","foaf:name":[{"@value":"Naoshi Hirata"}]}],"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":"1996-10-15","prism:volume":"23","prism:number":"21","prism:startingPage":"3067","prism:endingPage":"3070"},"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%2F96GL02765"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/96GL02765"}],"createdAt":"2004-02-04","modifiedAt":"2023-11-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360285704779361280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deep slab dehydration and large‐scale upwelling flow in the upper mantle beneath the Japan Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707402276864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"3D upper mantle structure beneath Japan and its surrounding region from inter-station dispersion measurements of surface waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707500184192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of the Sea of Japan back-arc and some unsolved issues"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166662444032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Quantifying crustal extension and shortening in the back‐arc region of Northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207166592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal Structure of the Trench-Island Arc-Back-arc Sea System from the Nankai Trough to the Northern Margin of the Yamato Basin, Southwest Japan"},{"@language":"ja","@value":"西南日本における海溝‐島弧‐縁海系の地殻構造―南海トラフから大和海盆北縁まで―"},{"@value":"西南日本における海溝-島弧-縁海系の地殻構造--南海トラフから大和海盆北縁まで"},{"@language":"ja-Kana","@value":"セイナン ニホン ニ オケル カイコウ トウ コ エンカイケイ ノ チカク コウゾウ ナンカイ トラフ カラ ヤマトカイボン ホクエン マデ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489392768","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"P-wave velocity structure in the northern part of the central Japan Basin, Japan Sea with ocean bottom seismometers and airguns"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842087904384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Lg wave propagation in the area around Japan : observations and simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317034590208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Lithosphere–asthenosphere boundary beneath the Sea of Japan from transdimensional inversion of S-receiver functions"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/96gl02765"},{"@type":"OPENAIRE","@value":"doi_dedup___::c74297eb96f463f9fa62c27323005e9c"},{"@type":"CROSSREF","@value":"10.1186/2197-4284-1-10_references_DOI_EalC7zFeiC4sILeoIRmbgH3pTg4"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01501-5_references_DOI_EalC7zFeiC4sILeoIRmbgH3pTg4"},{"@type":"CROSSREF","@value":"10.1002/2014jb011781_references_DOI_EalC7zFeiC4sILeoIRmbgH3pTg4"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2010.02.012_references_DOI_EalC7zFeiC4sILeoIRmbgH3pTg4"},{"@type":"CROSSREF","@value":"10.1029/2011jb008355_references_DOI_EalC7zFeiC4sILeoIRmbgH3pTg4"},{"@type":"CROSSREF","@value":"10.1186/bf03352509_references_DOI_EalC7zFeiC4sILeoIRmbgH3pTg4"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2016.08.020_references_DOI_EalC7zFeiC4sILeoIRmbgH3pTg4"},{"@type":"CROSSREF","@value":"10.5026/jgeography.119.235_references_DOI_EalC7zFeiC4sILeoIRmbgH3pTg4"}]}