{"@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/1390845713048404352.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.5575/geosoc.2018.0029"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"029349013"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/029349013"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I029349013"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/geosoc/124/10/124_2018.0029/_pdf"}},{"identifier":{"@type":"NAID","@value":"130007578074"}}],"dc:title":[{"@language":"en","@value":"Zircon fission-track and U-Pb ages of the Green Tuff in Nishiwaga Town, Iwate Prefecture, and their implications"},{"@language":"ja","@value":"岩手県西和賀町に分布するグリーンタフのジルコンFTおよびU-Pb年代とその意味"},{"@language":"ja-Kana","@value":"イワテケン ニシワガマチ ニ ブンプ スル グリーンタフ ノ ジルコン FT オヨビ U-Pb ネンダイ ト ソノ イミ"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"<p>We carried out fission-track (FT) and U-Pb double dating on zircon grains from six Green Tuff samples collected from Nishiwaga Town, Iwate Prefecture (northeast Japan). Based on these data, our revised stratigraphy is as follows: the Oarasawa Formation (the early Miocene ca. 20-18 Ma), which unconformably overlies the Paleozoic and Mesozoic basement; the main part of the Oishi Formation (16-15.4 Ma), which unconformably overlies the Oarasawa Formation; the Kawashiri Tuff Member (15.4-13.6 Ma) of the upper part of the Oishi Formation; and the Kotsunagizawa Formation (13.6-12 Ma), which conformably overlies the Oishi Formation. These results, which are consistent with the recently revised stratigraphy for the type section of the Green Tuff on Oga Peninsula, indicate that a tectonic change which is coupled with rapid tectonic subsidence started at ca. 16 Ma, accompanied by active felsic volcanism and counter-clockwise rotation of the region at ca. about 15.4-13.6 Ma, and then ended at ca. 12 Ma in the study area.</p>"},{"@language":"ja","@value":"<p>岩手県西和賀町周辺に分布するグリーンタフについて，ジルコンFTおよびU-Pbダブル年代測定を実施し，本地域のグリーンタフ層序と堆積年代を再検討した．堆積年代は下位から順に，大荒沢層（20-18Ma），大荒沢層を不整合に被覆する大石層主部（16-15.4Ma），大石層上部に相当する川尻凝灰岩部層（15.4-13.6Ma），大石層を整合に覆う小繋沢層（13.6-12Ma）と推定した．この結果は，近年改訂されたグリーンタフの模式層序の年代と調和的である．本調査地域は16Ma頃にテクトニクスが変化し，急速に沈降した．この変化は15.4-13.6Ma頃に活発な珪長質火山活動と調査地域の回転運動を伴って，12Ma頃に収束した．</p>"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420001326222077440","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"50760196"},{"@type":"NRID","@value":"1000050760196"},{"@type":"NRID","@value":"9000414254679"},{"@type":"NRID","@value":"9000404112236"},{"@type":"NRID","@value":"9000365617738"},{"@type":"NRID","@value":"9000414254697"},{"@type":"NRID","@value":"9000399496704"},{"@type":"NRID","@value":"9000242676535"},{"@type":"NRID","@value":"9000406354361"},{"@type":"NRID","@value":"9000258216224"},{"@type":"NRID","@value":"9000006894253"},{"@type":"NRID","@value":"9000021795731"},{"@type":"NRID","@value":"9000243881707"},{"@type":"NRID","@value":"9000405873319"},{"@type":"NRID","@value":"9000240048373"},{"@type":"NRID","@value":"9000403544897"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/jun_hosoi"}],"foaf:name":[{"@language":"en","@value":"Hosoi 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Takafumi"},{"@language":"ja","@value":"平田 岳史"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Geochemical Research Center, The University of Tokyo"},{"@language":"ja","@value":"東京大学大学院理学系研究科附属地殻化学実験施設"}]},{"@id":"https://cir.nii.ac.jp/crid/1410845713048404357","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000399496709"}],"foaf:name":[{"@language":"en","@value":"Amano Kazuo"},{"@language":"ja","@value":"天野 一男"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"日本大学文理学部自然科学研究所"},{"@language":"en","@value":"The Institute of National Sciences, College of Humanities and Sciences, Nihon 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Geol. Soc. Japan"},{"@language":"ja","@value":"地質雑"},{"@language":"ja","@value":"地雑"}],"dc:publisher":[{"@language":"en","@value":"The Geological Society of Japan"},{"@language":"ja","@value":"一般社団法人 日本地質学会"}],"prism:publicationDate":"2018-10-15","prism:volume":"124","prism:number":"10","prism:startingPage":"819","prism:endingPage":"835"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/029349013"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I029349013"},{"@id":"https://www.jstage.jst.go.jp/article/geosoc/124/10/124_2018.0029/_pdf"}],"availableAt":"2018-10-15","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Green%20tuff","dc:title":"Green tuff"},{"@id":"https://cir.nii.ac.jp/all?q=Miocene","dc:title":"Miocene"},{"@id":"https://cir.nii.ac.jp/all?q=fisson-track%20age","dc:title":"fisson-track age"},{"@id":"https://cir.nii.ac.jp/all?q=U-Pb%20age","dc:title":"U-Pb age"},{"@id":"https://cir.nii.ac.jp/all?q=double%20dating","dc:title":"double dating"},{"@id":"https://cir.nii.ac.jp/all?q=zircon","dc:title":"zircon"},{"@id":"https://cir.nii.ac.jp/all?q=Green%20tuff","dc:title":"Green tuff"},{"@id":"https://cir.nii.ac.jp/all?q=Miocene","dc:title":"Miocene"},{"@id":"https://cir.nii.ac.jp/all?q=fisson-track%20age","dc:title":"fisson-track age"},{"@id":"https://cir.nii.ac.jp/all?q=U%E2%80%93Pb%20age","dc:title":"U–Pb age"},{"@id":"https://cir.nii.ac.jp/all?q=double%20dating","dc:title":"double dating"},{"@id":"https://cir.nii.ac.jp/all?q=zircon","dc:title":"zircon"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002218164275712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An inter‐laboratory evaluation of <scp>OD</scp>‐3 zircon for use as a secondary <scp><scp>U–Pb</scp></scp> dating standard"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142939719296","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"THREE NATURAL ZIRCON STANDARDS FOR U‐TH‐PB, LU‐HF, TRACE ELEMENT AND REE ANALYSES"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168817644160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Age and associated stress field of middle Miocene back‐arc basalt magmatism in Northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710504477056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Paleomagnetic constraints on <scp>M</scp>iocene rotation in the central <scp>J</scp>apan <scp>A</scp>rc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617911078144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Standardization of fission track dating calibration: Recommendation by the Fission Track Working Group of the I.U.G.S. 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