{"@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/1360004234027477632.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1080/00206814.2017.1379912"}},{"identifier":{"@type":"URI","@value":"https://www.tandfonline.com/doi/pdf/10.1080/00206814.2017.1379912"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Direct ascent to the surface of asthenospheric magma in a region of convex lithospheric flexure"}],"description":[{"notation":[{"@value":"ABSTRACTThe stress field of oceanic lithosphere controls the distribution of submarine petit-spot volcanoes. However, the eruption sites of these petit-spot volcanoes are considered to be limited to concavely flexed regions of lithosphere off the outer rise. Here, we present new data for a recently identified petit-spot lava field on a convexly flexed section of the lithosphere adjacent to the subduction zone offshore of northeast Japan in an area containing more than 80 volcanoes. This area is marked by strongly alkaline lavas that were erupted on the convexly flexed region. As for the concavely flexed region where the petit-spots previously reported, the base of the lithosphere beneath the eruption sites is under extension, whereas the upper part of the lithosphere is under compression. This change in the stress field, from the lower to upper lithosphere, causes ascending dikes to stall in the mid-lithosphere, leading to metasomatic interaction with the surrounding peridotite. The new geochemical data o..."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004234027477632","@type":"Researcher","foaf:name":[{"@value":"Yuki Sato"}],"jpcoar:affiliationName":[{"@value":"Department of Earth Science, Graduate School of Science, Tohoku University, Sendai, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801181841024","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"00451831"},{"@type":"NRID","@value":"1000000451831"},{"@type":"CINII_AUTHOR_ID","@value":"DA19622571"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA19622571#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA19622571"},{"@type":"NRID","@value":"9000004600934"},{"@type":"NRID","@value":"9000345296010"},{"@type":"NRID","@value":"9000397671750"},{"@type":"NRID","@value":"9000258406875"},{"@type":"NRID","@value":"9000347135683"},{"@type":"NRID","@value":"9000345427350"},{"@type":"NRID","@value":"9000317558323"},{"@type":"NRID","@value":"9000403550563"},{"@type":"NRID","@value":"9000004600938"},{"@type":"NRID","@value":"9000396138837"},{"@type":"NRID","@value":"9000403550342"},{"@type":"NRID","@value":"9000347226909"},{"@type":"NRID","@value":"9000010418068"},{"@type":"NRID","@value":"9000241432997"},{"@type":"NRID","@value":"9000347187686"},{"@type":"NRID","@value":"9000345296248"},{"@type":"NRID","@value":"9000406396141"},{"@type":"NRID","@value":"9000010353648"},{"@type":"NRID","@value":"9000369737046"},{"@type":"NRID","@value":"9000345296046"},{"@type":"NRID","@value":"9000386336903"},{"@type":"NRID","@value":"9000345439022"},{"@type":"NRID","@value":"9000403552000"},{"@type":"NRID","@value":"9000007158097"},{"@type":"NRID","@value":"9000343409924"},{"@type":"NRID","@value":"9000283905501"},{"@type":"NRID","@value":"9000338418883"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/nhirano"}],"foaf:name":[{"@value":"Naoto 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Nakanishi"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Science, Chiba University, Chiba, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004234027477378","@type":"Researcher","foaf:name":[{"@value":"Teruaki Ishii"}],"jpcoar:affiliationName":[{"@value":"Center for Integrated Research and Education of Natural Hazards, Shizuoka University, Shizuoka, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004234027477634","@type":"Researcher","foaf:name":[{"@value":"Arashi Taki"}],"jpcoar:affiliationName":[{"@value":"Department of Earth Science, Graduate School of Science, Tohoku University, Sendai, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004234027477377","@type":"Researcher","foaf:name":[{"@value":"Kazutaka Yasukawa"}],"jpcoar:affiliationName":[{"@value":"Department of Systems Innovation, School of Engineering, The University of Tokyo, Tokyo, Japan"},{"@value":"Ocean Resources Research Center for Next Generation, Chiba Institute of Technology, Chiba, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004234027477635","@type":"Researcher","foaf:name":[{"@value":"Yasuhiro Kato"}],"jpcoar:affiliationName":[{"@value":"Department of Systems Innovation, School of Engineering, The University of Tokyo, Tokyo, Japan"},{"@value":"Ocean Resources Research Center for Next Generation, Chiba Institute of Technology, Chiba, Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00206814"},{"@type":"EISSN","@value":"19382839"}],"prism:publicationName":[{"@value":"International Geology Review"}],"dc:publisher":[{"@value":"Informa UK Limited"}],"prism:publicationDate":"2017-09-27","prism:volume":"60","prism:number":"10","prism:startingPage":"1231","prism:endingPage":"1243"},"reviewed":"false","url":[{"@id":"https://www.tandfonline.com/doi/pdf/10.1080/00206814.2017.1379912"}],"createdAt":"2017-09-27","modifiedAt":"2020-08-18","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781965828864","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"17K05715"},{"@type":"JGN","@value":"JP17K05715"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-17K05715/"}],"notation":[{"@language":"ja","@value":"海底岩石から直接読み解く沈み込むプレートの変動履歴"},{"@language":"en","@value":"Tectonic process resolved by geochemistry of submarine basalts"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000781974732288","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"17K18794"},{"@type":"JGN","@value":"JP17K18794"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-17K18794/"}],"notation":[{"@language":"ja","@value":"ピコモル炭素に適用できる新たな炭素同位体比測定法の開発"},{"@language":"en","@value":"Development of a new analysis method for isotope ratios of pico-mole carbon"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000781998331264","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"18K03772"},{"@type":"JGN","@value":"JP18K03772"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-18K03772/"}],"notation":[{"@language":"ja","@value":"白亜紀太平洋のおけるテクトニクス事変からみたプレート運動駆動力"},{"@language":"en","@value":"Plate driving force of the Cretaceous Pacific Plate"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256805970304","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H03720"},{"@type":"JGN","@value":"JP15H03720"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H03720/"}],"notation":[{"@language":"ja","@value":"巨大海台の正体を探る：海底地震・電磁気観測によるオントンジャワ海台地下構造の推定"},{"@language":"en","@value":"Exploring Large Igneous Provinces: Determination of crust and mantle structure beneath the Ontong Java Plateau by marine geophysical observation"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256821596928","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15K05261"},{"@type":"JGN","@value":"JP15K05261"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15K05261/"}],"notation":[{"@language":"ja","@value":"白亜紀中期太平洋におけるプレート境界再配列と拡大速度から見たプレート運動の駆動力"},{"@language":"en","@value":"The driving force of the plate motion based on the plate reorganization of plate boundaries surrounding the Cretaceous Pacific Plate and spreading rates"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256875821184","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H04079"},{"@type":"JGN","@value":"JP16H04079"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16H04079/"}],"notation":[{"@language":"ja","@value":"マントルウェッジ炭素の起源をさぐる"},{"@language":"en","@value":"The origin of mantle wedge carbon"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256932958592","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"17H02975"},{"@type":"JGN","@value":"JP17H02975"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-17H02975/"}],"notation":[{"@language":"ja","@value":"溶融宇宙塵から復元する大気酸素同位体比と生物生産の変動"},{"@language":"en","@value":"Reconstruction of atmospheric oxygen isotope composition using ancient cosmic spherules"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256969297024","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"18H01303"},{"@type":"JGN","@value":"JP18H01303"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-18H01303/"}],"notation":[{"@language":"ja","@value":"MOWALL:トランスフォーム断層で海洋地殻生産プロセスの時空間変動を追う"},{"@language":"en","@value":"MOWALL: Moho Observation along transform fault WALLs"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050025031481019008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Thermal structure beneath Far Eastern Russia inferred from geothermobarometric analyses of mantle xenoliths: Direct evidence for high geothermal gradient in backarc lithosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1050587981428475520","@type":"Article","resourceType":"学術雑誌論文(journal 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