{"@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/1362825896165724928.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/1999gl011080"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F1999GL011080"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/1999GL011080"}}],"dc:title":[{"@value":"Seismological evidence for the existence of serpentinized wedge mantle"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Serpentinized peridotite is detected seismologically by mapping Poisson's ratio beneath the Kanto district, central Japan, because serpentinite has a higher Poisson's ratio than other rocks in the crust and upper mantle. We determine three‐dimensional P and S wave velocity models using travel time tomography and then construct a three‐dimensional map of Poisson';s ratio. The models show low velocity anomalies near the upper boundary of the slab in a depth range from 20 to 70 km. In the low velocity region, there is an area with Poisson's ratio greater than 0.3 at depths of 20–45 km, which we attribute to serpentinized peridotite. The rest of the low velocity region is interpreted as descending oceanic crust with a Poisson's ratio of about 0.25. The high Poisson's ratio area is associated with low seismicity and weak interplate coupling, which is consistent with the ductility of serpentinite.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825896165724929","@type":"Researcher","foaf:name":[{"@value":"Shin'ichiro Kamiya"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896165724928","@type":"Researcher","foaf:name":[{"@value":"Yoji Kobayashi"}]}],"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":"2000-03-15","prism:volume":"27","prism:number":"6","prism:startingPage":"819","prism:endingPage":"822"},"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%2F1999GL011080"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/1999GL011080"}],"createdAt":"2002-09-17","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050012570393792000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tomographic image of crust and upper mantle off the Boso Peninsula using data from an ocean-bottom seismograph array"}]},{"@id":"https://cir.nii.ac.jp/crid/1050564288821961472","@type":"Article","resourceType":"学術雑誌論文(journal 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Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707150643200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geochemical mapping of slab-derived fluid and source mantle along Japan arcs"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708266750592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical conductivity of magnetite‐bearing serpentinite during shear deformation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643725324288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Major Mineral Fraction and Physical Properties of Carbonated Peridotite (Listvenite) From ICDP Oman Drilling Project Hole BT1B Inferred From X‐Ray CT Core Images"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165262658304","@type":"Article","resourceType":"学術雑誌論文(journal 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スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206458511104","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-dimensional P and S Wave Velocity Structure beneath Central Japan."},{"@language":"ja","@value":"中部日本の３次元速度構造"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496439296","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地殻・上部マントルでの減衰<br/>─トモグラフィ手法によるQ値評価とその利用─"},{"@language":"en","@value":"Attenuation structure at crust and upper mantle<br/>—Estimation of Q<sub>s</sub>-value by tomographic analysis and its applications—"},{"@value":"地殻・上部マントルでの減衰 : トモグラフィ手法によるQ値評価とその利用"},{"@language":"ja-Kana","@value":"チカク ・ ジョウブ マントル デ ノ ゲンスイ : トモグラフィ シュホウ ニ ヨル Qチ ヒョウカ ト ソノ リヨウ"},{"@value":"Attenuation structure at crust and upper mantle<br/>&mdash;Estimation of Q<sub>s</sub>-value by tomographic analysis and its 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Peninsula, central Honshu, Japan—"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206525915136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Effect of pore fluid pressure on elastic wave velocities of serpentinites"},{"@language":"ja","@value":"蛇紋岩の弾性波速度に対する間隙水圧の影響"},{"@language":"ja-Kana","@value":"ジャモンガン ノ ダンセイハ ソクド ニ タイスル カンゲキ スイアツ ノ エイキョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390016681646568448","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"3-D S-wave Attenuation Structure beneath the Kanto Region, Japan, Retrieved by Spectrum Inversion"},{"@language":"ja","@value":"スペクトルインバージョンによって推定された関東地域の三次元S波減衰構造"},{"@language":"ja-Kana","@value":"スペクトルインバージョン ニ ヨッテ スイテイ サレタ カントウ チイキ ノ サンジゲン Sハ ゲンスイ コウゾウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207162752","@type":"Article","resourceType":"学術雑誌論文(journal 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Significance"},{"@language":"ja-Kana","@value":"ジャモンガン ノ リキガクテキ セイシツ ト ソノ テクトニック ナ イギ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679279748096","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismic Velocity and Electrical Conductivity of Rocks in the Crust and Mantle: Probing Water in Subduction Zones"},{"@language":"ja","@value":"地殻・マントル物質の地震波速度と電気伝導度：沈み込み帯の水を探る"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489663360","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismic tomography of the uppermost mantle beneath southwestern Japan: Seismological constraints on modelling subduction and magmatism for the Philippine Sea slab"},{"@value":"Seismic tomography of the uppermost mantle beneath southwestern Japan: seismological constraints on modeling subduction and magmatism for the Philippine Sea Slab"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681490297728","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Dehydration of serpentinized slab mantle: Seismic evidence from southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681503323008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A recent trend in sciences on mantle-derived materials, with special emphases on refertilization, rheology, and ophiolite problems: a report of the Fifth International Conference on Orogenic Lherzolite"},{"@language":"ja","@value":"マントル科学研究の最近の動向‐特に再肥沃化，レオロジー，オフィオライト問題：第５回国際レルゾライト会議報告"},{"@value":"マントル科学研究の最近の動向--特に再肥沃化,レオロジー,オフィオライト問題--第5回国際レルゾライト会議報告"},{"@language":"ja-Kana","@value":"マントル カガク ケンキュウ ノ サイキン ノ ドウコウ トクニ サイヒヨクカ レオロジー オフィオライト モンダイ ダイ5カイ コクサイ レルゾライト カイギ 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