{"@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/1362544420171474432.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0012-821x(96)00023-4"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0012821X96000234?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0012821X96000234?httpAccept=text/plain"}}],"dc:title":[{"@value":"The influence of trench migration on slab penetration into the lower mantle"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382544420171474432","@type":"Researcher","foaf:name":[{"@value":"Ulrich R. Christensen"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0012821X"}],"prism:publicationName":[{"@value":"Earth and Planetary Science Letters"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1996-05","prism:volume":"140","prism:number":"1-4","prism:startingPage":"27","prism:endingPage":"39"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","http://creativecommons.org/licenses/by-nc-nd/4.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:0012821X96000234?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:0012821X96000234?httpAccept=text/plain"}],"createdAt":"2002-07-25","modifiedAt":"2019-04-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050012570393434752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three‐dimensional numerical modeling of temperature and mantle flow fields associated with subduction of the Philippine Sea plate, southwest Japan"},{"@value":"Three-dimensional numerical modeling of temperature and mantle flow fields associated with subduction of the Philippine Sea plate, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050294045370471424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three‐dimensional numerical modeling of thermal regime and slab dehydration beneath Kanto and Tohoku, Japan"},{"@value":"Three-dimensional numerical modeling of thermal regime and slab dehydration beneath Kanto and Tohoku, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050575520347085696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Effects of slab geometry and obliquity on the interplate thermal regime associated with the subduction of three-dimensionally curved oceanic plates"}]},{"@id":"https://cir.nii.ac.jp/crid/1050575520348931968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Interrelation of the stagnant slab, Ontong Java Plateau, and intraplate volcanism as inferred from seismic tomography"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214348529024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Subducted slabs stagnant above, penetrating through, and trapped below the 660 km discontinuity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216113765632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geophysical and mineralogical constraints on the post-spinel transformation for the Tonga slab"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233285030016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Basaltic accumulation instability and chaotic plate motion in the earliest mantle inferred from numerical experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707150737920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Conjecture with water and rheological control for subducting slab in the mantle transition zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165869769088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of water transportation on subduction dynamics: Roles of viscosity and density reduction"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179759080320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Slab pileup in the mantle transition zone and the 30 May 2015 Chichi‐jima earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181859862272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamics of Subducting Slabs: Numerical Modeling and Constraints from Seismology, Geoid, Topography, Geochemistry, and Petrology"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182379017728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"On the possibility of a folded crustal layer stored in the hydrous mantle transition zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580230590435712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermal regime and slab dehydration beneath the Izu‐Bonin arc: Implications for fast and slow subduction earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584341824297472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Cubic Fe-bearing majorite synthesized at 18–25 GPa and 1000 °C: implications for element transport, subducted slab rheology and diamond formation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640846340736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamics of slab rollback and induced back-arc basin formation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641639212160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The 3D numerical modeling of subduction dynamics: Plate stagnation and segmentation, and crustal advection in the wet mantle transition zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567354796672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"2-D Numerical Simulations on Formation and Descent of Stagnant Slabs: Important Roles of Trench Migration and Its Temporal Change"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861705569327872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Subduction-zone parameters that control slab behavior at the 660-km discontinuity revealed by logistic regression analysis and model selection"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855104043008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of Hot Plumes and Slab Rheology on the Bending of the Philippine Sea Slab at Shallow Depths Beneath the Kyushu Region, Southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694368032244992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three‐Dimensional <i>S</i> Velocity Structure of the Mantle Transition Zone Beneath Central America and the Gulf of Mexico Inferred Using Waveform Inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204238418944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地球型惑星内部物理学の最近の進展"},{"@language":"en","@value":"Recent Advances in Geophysical Studies of the Interior of Terrestrial Planets"},{"@language":"ja-Kana","@value":"チキュウガタ ワクセイ ナイブ ブツリガク ノ サイキン ノ シンテン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303003136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A Present State and Perspective on Numerical Simulation Studies of Stagnant Slabs"},{"@language":"ja","@value":"滞留スラブの数値シミュレーション研究の現状と今後の展望"},{"@language":"ja-Kana","@value":"タイリュウ スラブ ノ スウチ シミュレーション ケンキュウ ノ ゲンジョウ ト コンゴ ノ テンボウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206508965376","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"NW Pacific slab rheology, the seismicity cutoff, and the olivine to spinel phase change"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681485713536","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mesoscale structures in the transition zone"},{"@value":"Mesoscale structures in the transition zone: Dynamical consequences of boundary layer activities"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417163391488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dominant role of temperature on deep earthquake mechanics for the Tonga slab near the bottom of the upper mantle"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/0012-821x(96)00023-4"},{"@type":"CROSSREF","@value":"10.1002/2013jb010466_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1186/bf03352192_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1186/s40623-014-0138-2_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1029/2008jb006222_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2016.08.016_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1002/2016jb012912_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2014.04.011_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1002/2016gl068168_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.10.031_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1111/ter.12568_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1038/s41598-021-99833-5_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1038/s41598-023-43037-6_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.21203/rs.3.rs-2582055/v1_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1029/2011jb008989_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1186/bf03352198_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1002/2016jb013230_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.265_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2013.03.004_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.3389/feart.2020.00117_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.3389/feart.2022.1008058_references_DOI_WQdoeRB3yTV5PgEpcZHAJBdaiBQ"},{"@type":"CROSSREF","@value":"10.1007/s00024-024-03616-8_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1029/2018jb016924_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.5026/jgeography.124.1_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1016/b978-0-444-53802-4.00132-9_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2012.02.009_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2013.12.005_references_DOI_EoWWXgNF3ClQokg7sLW40qG33ov"}]}