{"@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/1360004232102685184.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.earscirev.2016.05.011"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012825216300988?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012825216300988?httpAccept=text/plain"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Formation and evolution of Shatsky Rise oceanic plateau: Insights from IODP Expedition 324 and recent geophysical cruises"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004232102685186","@type":"Researcher","foaf:name":[{"@value":"William W. Sager"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232102685185","@type":"Researcher","foaf:name":[{"@value":"Takashi Sano"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232102685184","@type":"Researcher","foaf:name":[{"@value":"Jörg Geldmacher"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00128252"}],"prism:publicationName":[{"@value":"Earth-Science Reviews"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2016-08","prism:volume":"159","prism:startingPage":"306","prism:endingPage":"336"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license","http://www.elsevier.com/open-access/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0012825216300988?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0012825216300988?httpAccept=text/plain"}],"createdAt":"2016-05-29","modifiedAt":"2025-11-02","project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257267131136","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26302010"},{"@type":"JGN","@value":"JP26302010"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26302010/"}],"notation":[{"@language":"ja","@value":"1億年間続く巨大海台のマグマ活動"},{"@language":"en","@value":"Detection of Oceanic Plateau magmatism lasting for ~100 million years"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002214348919680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ocean <scp>B</scp>asalt <scp>S</scp>imulator version 1 (<scp>OBS</scp>1): Trace element mass balance in adiabatic melting of a pyroxenite‐bearing peridotite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216709518080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Variety and origin of magmas on Shatsky Rise, northwest Pacific Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142646703744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Two-stages of plume tail volcanism formed Ojin Rise Seamounts adjoining Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143747800320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Volatiles in Submarine Basaltic Glasses from the Northern Kerguelen Plateau (ODP Site 1140): Implications for Source Region Compositions, Magmatic Processes, and Plateau Subsidence"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143865648384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geothermobarometry of basaltic glasses from the Tamu Massif, Shatsky Rise oceanic plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144280326400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Petrology of Lavas from the Lamont Seamount Chain and Adjacent East Pacific Rise, 10  N"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144364035712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Some physical requirements for the emplacement of long basaltic lava flows"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144756827648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lead isotopes reveal bilateral asymmetry and vertical continuity in the Hawaiian mantle plume"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144781903360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rapid formation of the Shatsky Rise oceanic plateau inferred from its magnetic anomaly"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144962236416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sequence stratigraphy, structure, and tectonic history of the southwestern Ontong Java Plateau adjacent to the North Solomon Trench and Solomon Islands Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145452557952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Iceland Mantle Plume: Geochemical Study of Reykjanes Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145759160320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Long-term interaction between mid-ocean ridges and mantle plumes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145996961024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dynamics of plume–triple junction interaction: Results from a series of three‐dimensional numerical models and implications for the formation of oceanic plateaus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146158823296","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Plumes in central Panthalassa? Deductions from accreted oceanic fragments in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146604616448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An immense shield volcano within the Shatsky Rise oceanic plateau, northwest Pacific Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021390563077504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The nature of the Pacific plate as subduction inputs to the northeastern Japan arc and its implication for subduction zone processes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707112038272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Paleo-elevation and subsidence of <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" altimg=\"si1.gif\" overflow=\"scroll\"><mml:mo>∼</mml:mo><mml:mn>145</mml:mn><mml:mspace width=\"0.25em\"/><mml:mtext>Ma</mml:mtext></mml:math> Shatsky Rise inferred from CO2 and H2O in fresh volcanic glass"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617623676800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magnetic Anomaly Map of Shatsky Rise and Its Implications for Oceanic Plateau Formation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617907759744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Broad plumes rooted at the base of the Earth's mantle beneath major hotspots"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617911557120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Sea Floor Topography from Satellite Altimetry and Ship Depth Soundings"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617915364736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A model for the global variation in oceanic depth and heat flow with lithospheric age"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292618627560704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mantle plumes: Thin, fat, successful, or failing? Constraints to explain hot spot volcanism through time and space"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619135784320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Melting phase relations of an anhydrous mid‐ocean ridge basalt from 3 to 20 GPa: Implications for the behavior of subducted oceanic crust in the mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619329452416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geochemical evidence for a mid-Cretaceous superplume"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620196727296","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Subsidence of the Kerguelen Plateau: The Atlantis Concept"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620892293248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Data report: paleomagnetic measurements of igneous rocks from Shatsky Rise Expedition 324"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620907307008","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Regional Syntheses, Line Islands Chain, Tuamotu Island Chain, and Manihiki Plateau, Central Pacific Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621314197120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Age and geochemistry of the oceanic Manihiki Plateau, SW Pacific: New evidence for a plume origin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621325824256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reconstructing Ontong Java Nui: Implications for Pacific absolute plate motion, hotspot drift and true polar wander"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298757423018880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Extracting the geochemical characteristics of magmas in different global tectono-magmatic settings using sparse modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302865722998272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Possible partial melting and production of felsic melt in a Jurassic oceanic plateau of the Izanagi Plate: Insights from 159 Ma plagiogranites from northern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088714880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The stable vanadium isotope composition of the mantle and mafic lavas"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092888813056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hikurangi Plateau: Crustal structure, rifted formation, and Gondwana subduction history"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094175720320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The age of Earth’s largest volcano: Tamu Massif on Shatsky Rise (northwest Pacific Ocean)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094527426560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Implications of mantle plume structure for the evolution of flood basalts"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094835986176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Wavefront healing renders deep plumes seismically invisible"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095005333376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Plumes, or plate tectonic processes?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095300402560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Changing Nature of Mantle Hotspots through Time: Implications for the Chemical Evolution of the Mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095595660160","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Basement reflectors in the Kerguelen Plateau, south Indian Ocean: Indications for the structure and early history of the plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096063720192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geochemistry of Lavas from the Emperor Seamounts, and the Geochemical Evolution of Hawaiian Magmatism from 85 to 42 Ma"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096159507328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geoid height versus topography for oceanic plateaus and swells"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640867372288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geochemistry and age of Shatsky, Hess, and Ojin Rise seamounts: Implications for a connection between the Shatsky and Hess Rises"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065732096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magnetic anomaly map of Ori Massif and its implications for oceanic plateau formation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848663510517376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Massive basalt flows on the southern flank of Tamu Massif, Shatsky Rise: a reappraisal of ODP Site 1213 basement units"}]},{"@id":"https://cir.nii.ac.jp/crid/1360849943286246912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Oceanic plateau formation by seafloor spreading implied by Tamu Massif magnetic anomalies"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567860209920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An analysis of the variation of ocean floor bathymetry and heat flow with age"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568630113536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569972839040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Manihiki Plateau—A multistage volcanic emplacement history"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571108012800","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Influence of spreading rate and magma supply on crystallization and assimilation beneath mid‐ocean ridges: Evidence from chlorine and major element chemistry of mid‐ocean ridge basalts"}]},{"@id":"https://cir.nii.ac.jp/crid/1360870485028428544","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Carbonation of oceanic serpentinite related to extensive intraplate magmatism"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043501794176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Origin of enriched ocean ridge basalts and implications for mantle dynamics"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044329036288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Numerical investigations of the mantle plume initiation model for flood basalt events"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044434447872","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An ancient recipe for flood-basalt genesis"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044932727552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"“Equator Crossing” of Shatsky Rise?: New insights on Shatsky Rise tectonic motion from the downhole magnetic architecture of the uppermost lava sequences at Tamu Massif"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045019768320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"How and when plume zonation appeared during the 132 Myr evolution of the Tristan Hotspot"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045027883520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Boron and chlorine contents of upper oceanic crust: Basement samples from IODP Hole 1256D"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045505753600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Plume versus plate origin for the Shatsky Rise oceanic plateau (NW Pacific): Insights from Nd, Pb and Hf isotopes"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045604558592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lead and Helium Isotope Evidence from Oceanic Basalts for a Common Deep Source of Mantle Plumes"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045682361344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Toward a self‐consistent, high‐resolution absolute plate motion model for the Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518485656704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mantle flow and melting beneath oceanic ridge–ridge–ridge triple junctions"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519599171072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A cool model for the Iceland hotspot"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520204921856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Kerguelen Hotspot Magma Output since 130 Ma"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520234654336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Interaction of mantle plume heads with the Earth's surface and onset of small‐scale convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520319535744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Top-Down Tectonics?"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520534682240","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Data report: magnetic properties of basalts from Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520757460480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Expedition 324 summary"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520895840640","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three distinct types of hotspots in the Earth’s mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418521175979776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Thermal and chemical structure of the Iceland plume"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418521380991360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Interaction between the Mid‐Atlantic Ridge and the Azores hot spot during the last 85 Myr: Emplacement and rifting of the hot spot‐derived plateaus"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993674967808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Testing the plume theory"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993819764096","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A POSSIBLE ORIGIN OF THE HAWAIIAN ISLANDS"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994430196736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stirring and structure in mantle starting plumes"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994437371648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A possible role for garnet pyroxenite in the origin of the \"garnet signature\" in MORB"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994462994560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Compensation of the Ontong Java Plateau by surface and subsurface loading"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995594224256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mafic volcaniclastic deposits in flood basalt provinces: A review"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699996417147904","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lithosphere, asthenosphere, and perisphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468711030016","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Correlations of Ocean Ridge Basalt Chemistry with Axial Depth: a New Perspective"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468715342848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hotspots, mantle plumes, flood basalts, and true polar wander"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468890055552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Plume Generation Zones at the margins of Large Low Shear Velocity Provinces on the core–mantle boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469051737600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mixing and deformations in mantle plumes"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469306741632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Plate Tectonics and Hotspots: The Third Dimension"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469445138304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Is \"Hotspot\" Volcanism a Consequence of Plate Tectonics?"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470081756544","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Major and trace element composition of the high <sup>3</sup>He/<sup>4</sup>He mantle: Implications for the composition of a nonchonditic Earth"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470197533568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reconstructing lava flow emplacement processes at the hot spot‐affected Galápagos Spreading Center, 95<sup>°</sup>W and 92<sup>°</sup>W"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470840820480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Melt generation by isentropic mantle upwelling"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981471461860096","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tectonic evolution of the northern Pacific plate and Pacific-Farallon Izanagi triple junction in the Late Jurassic and Early Cretaceous (M21-M10)"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943483017088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Beyond the thermal plume paradigm"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943559251584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Large volume recycling of oceanic lithosphere over short time scales: geochemical constraints from the Caribbean Large Igneous Province"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943579112448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Samoan hot spot track on a “hot spot highway”: Implications for mantle plumes and a deep Samoan mantle source"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943842491648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Volume and Composition of Melt Generated by Extension of the Lithosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944599035648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An assessment of local and regional isotopic equilibrium in the mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944987619712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Models of earth structure inferred from neodymium and strontium isotopic abundances"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945114568832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Shape analysis of Pacific seamounts"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945287326720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Bathymetry of Shatsky Rise, northwest Pacific Ocean: Implications for ocean plateau development at a triple junction"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945288142592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mantle Plumes and Entrainment: Isotopic Evidence"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945463997184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Low-buoyancy thermochemical plumes resolve controversy of classical mantle plume concept"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945639006080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Galapagos Rift at 86° W: 3. Sheet flows, collapse pits, and lava lakes of the Rift Valley"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945918761216","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Layered Lithospheric Mantle Beneath the Ontong Java Plateau: Implications from Xenoliths in Alnöite, Malaita, Solomon Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946121936768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mantle plume tomography"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419200061952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hotspot trails in the South Atlantic controlled by plume and plate tectonic processes"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419398205568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geological consequences of superplumes"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419494731264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Agulhas Plateau: structure and evolution of a Large Igneous Province"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419948201984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic response and construction of seaward dipping wedges of flood basalts: Vøring volcanic margin"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420041631488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Finite-Frequency Tomography Reveals a Variety of Plumes in the Mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420892212864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Posterosional volcanism in the Cretaceous part of the Hawaiian Hotspot Trail"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421134322304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rapid Formation of Ontong Java Plateau by Aptian Mantle Plume Volcanism"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893493900672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Simultaneous generation of hotspots and superswells by convection in a heterogeneous planetary mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894110206976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Helium isotopic systematics of oceanic islands and mantle heterogeneity"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894140019712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Basement Geochemistry and Geochronology of Central Malaita, Solomon Islands, with Implications for the Origin and Evolution of the Ontong Java Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894377560576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Revised definition of Large Igneous Provinces (LIPs)"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894486965248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Origin of seaward-dipping reflectors in oceanic crust off the Norwegian margin by “subaerial sea-floor spreading”"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894508936064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mantle plumes: Why the current skepticism?"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894799969792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The largest volcanic eruptions on Earth"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894874682624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Convection Plumes in the Lower Mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895267984384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Upper mantle heterogeneities and dynamics"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895543413248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Data report: alteration of basalts from Sites U1346 and U1349 at Shatsky Rise oceanic plateau, IODP Expedition 324"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895809800064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Playing jigsaw with Large Igneous Provinces—A plate tectonic reconstruction of Ontong Java Nui, West Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895950967168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"How Do Oceanic Plateaus Form? Clues From Drilling at Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895955909376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Double Flood Basalts and Plume Head Separation at the 660-Kilometer Discontinuity"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825896078728960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Palaeointensity determinations and rock magnetic properties on basalts from Shatsky Rise: new evidence for a Mesozoic dipole low"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825896212191232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A catalogue of deep mantle plumes: New results from finite‐frequency tomography"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368350371712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Why did not the Ontong Java Plateau form subaerially?"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368451023744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"IODP Expedition 324: Ocean Drilling at Shatsky Rise Gives Clues about Oceanic Plateau Formation"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368561196288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Large Igneous Provinces and the Mantle Plume Hypothesis"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368855766912","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Paleomagnetic Evidence for Motion of the Pacific Plate from Leg 32 Basalts and Magnetic Anomalies"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369167075712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Data report: hysteresis measurements on basalts from Holes U1346A, U1347A, and U1350A on Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369249459712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Age and Geochemistry of Basement and Alkalic Rocks of Malaita and Santa Isabel, Solomon Islands, Southern Margin of Ontong Java Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369337464192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Perspective on the Genesis of E-MORB from Chemical and Isotopic Heterogeneity at 9–10°N East Pacific Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369375079168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The seismic Moho structure of Shatsky Rise oceanic plateau, northwest Pacific Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369462561280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structure and tectonic history of the Southern Kerguelen Plateau (Indian Ocean) deduced from seismic reflection data"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369582830720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"HOTSPOT SWELLS"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369833466624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The single largest oceanic plateau: Ontong Java–Manihiki–Hikurangi"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369837265280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Late Cretaceous genesis of the Kula plate"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370714942464","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic volcanostratigraphy of large‐volume basaltic extrusive complexes on rifted margins"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107371038140672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Anomalous uplift and subsidence of the Ontong Java Plateau inferred from CO2 contents of submarine basaltic glasses"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107371112372992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Subsidence and growth of Pacific Cretaceous plateaus"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107371147042048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A source for Icelandic magmas in remelted Iapetus crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107371180910592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mantle updrafts and mechanisms of oceanic volcanism"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843994157312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Large igneous provinces generated from the margins of the large low-velocity provinces in the deep mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844284916864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Flood Basalts and Hot-Spot Tracks: Plume Heads and Tails"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844772427520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetic lineations within Shatsky Rise, northwest Pacific Ocean: Implications for hot spot‐triple junction interaction and oceanic plateau formation"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845090656512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Cretaceous paleomagnetic apparent polar wander path for the Pacific plate calculated from Deep Sea Drilling Project and Ocean Drilling Program basalt cores"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845236902912","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the relationship between volcanic hotspot locations, the reconstructed eruption sites of large igneous provinces and deep mantle seismic structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845484794624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Intrabasement reflections of the Ontong Java Plateau: Implications for plateau construction"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388846266964992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Jurassic-Cretaceous boundary age and mid-ocean-ridge–type mantle source for Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318773701888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A statistical analysis of the correlation between large igneous provinces and lower mantle seismic structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318848162816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Existence of complex spatial zonation in the Galápagos plume"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319824960896","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evidence for an age progression along the Tristan-Gough volcanic track from new 40Ar/39Ar ages on phenocryst phases"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320014695424","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"70 m.y. history (139–69 Ma) for the Caribbean large igneous province"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320576316672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seaward dipping reflectors and the continent-ocean boundary at passive continental margins"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320794425344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"LINKS BETWEEN LONG‐LIVED HOT SPOTS, MANTLE PLUMES, D″, AND PLATE TECTONICS"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320857452160","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional passive flow and temperature structure beneath oceanic ridge–ridge–ridge triple junctions"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793339889920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Jurassic plume-origin ophiolites in Japan: accreted fragments of oceanic plateaus"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794204383488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The anatomy of Continental Flood Basalt Provinces: geological constraints on the processes and products of flood volcanism"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794226337664","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Multiple volcanic episodes of flood basalts caused by thermochemical mantle plumes"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794740332800","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Data report: underway geophysics"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795095534336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Large igneous provinces: Crustal structure, dimensions, and external consequences"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951796234276352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Observational and theoretical studies of the dynamics of mantle plume–mid‐ocean ridge interaction"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269233555712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Effect of H2O and Pressure on Multiple Saturation and Liquid Lines of Descent in Basalt from the Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269248511872","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An emerging palaeoceanographic ‘missing link’: multidisciplinary study of rarely recovered parts of deep-sea Santonian–Campanian transition from Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270066599552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Explosive Deep Water Basalt in the Sumisu Backarc Rift"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270090486528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the anatomy of mantle plumes: effect of the viscosity ratio on entrainment and stirring"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270247928704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mantle Sources and the Highly Variable Role of Continental Lithosphere in Basalt Petrogenesis of the Kerguelen Plateau and Broken Ridge LIP: Results from ODP Leg 183"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270716431360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Composition and timing of carbonate vein precipitation within the igneous basement of the Early Cretaceous Shatsky Rise, NW Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683229830","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lithium isotopic evidence for magmatic assimilation of hydrothermally influenced crust beneath oceanic large igneous provinces"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683229833","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Large mafic magmatic events through time and their links to mantle plume heads"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683229952","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geochemistry and geochronology of Leg 130 basement lavas: nature and origin of the Ontong Java Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683229953","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reorganization of the Pacific-Izanagi-Farallon triple junction in the Late Jurassic: tectonic events before the formation of Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683229957","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deep mantle convection plumes and plate motions"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683229962","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sampling mantle heterogeneity through oceanic basalts: isotopes and trace elements"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683229966","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Leg 183 synthesis: Kerguelen Plateau-Broken Ridge — a large igneous province"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683229968","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Basalts of the Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230085","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Paleomagnetism of the igneous section, Hole 1213B, Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230210","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Volcanic evolution of the submarine super volcano, Tamu Massif of Shatsky Rise: new insights from Formation Microscanner logging imagery"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230217","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Paleomagnetism of Early Cretaceous (Berriasian) sedimentary rocks, Hole 1213B, Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230218","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Accretionary-lapilli-bearing volcaniclastic rocks at ODP Site 1184: a record of subaerial phreatomagmatic eruptions on the Ontong Java Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230219","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Site U1349"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230222","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Leg 191 synthesis: summary of scientific results"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230341","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Morphology of Shatsky Rise oceanic plateau from high resolution bathymetry"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230345","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mesozoic sea-floor spreading in the north Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230347","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quantitative evaluation of element mobility during seawater alteration of basalts: an example from the Shatsky Rise oceanic plateau, NW Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230464","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evolution of the Vøring volcanic margin"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230466","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hyaloclastite from Miocene seamounts offshore central California: compositions, eruptions styles, and depositional processes"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230467","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Paleolatitudes and tectonic reconstructions of the oldest portion of the Pacific plate: a comparative study"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230468","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Pin-pricking the elephant: evidence on the origin of the Ontong Java Plateau from Pb-Sr-Hf-Nd isotopic characteristics of ODP Leg 192 basalts"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230471","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Failure to reject: testing the correlation beteen large igneous provinces and deep mantle structures with EDF statistics"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230475","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Leg 183 summary: Kerguelen Plateau-Broken Ridge — a large igneous province"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230477","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Appliation of the 2-D continuous wavelet transforms to imaging of Shatsky Rise plateau using marine seismic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230593","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic properties of flood basalts on rifted volcanic margins based on Ocean Drilling Program (ODP) Hole 917A downhole data"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230596","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Petrological systematics of mid-ocean ridge basalts: Constraints on melt generation beneath ocean ridges"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230601","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Crustal structure along the Leg 152 drilling transect"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230722","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Site U1347"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230723","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tectonic constraints on the hot-spot formation of Ninetyeast Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230724","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Implications for magmatic processes at Ontong Java Plateau from volatile and major elements contents of Cretaceous basalt glasses"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230725","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Volatiles in basaltic magmas from the Ontong Java Plateau: implications for mantle source regions, shallow level magmatic processes, and plateau subsidence"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230726","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Genesis of the Iceland melt anomaly by plate tectonic processes"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230728","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Isotope topology of individual hotspot basalt arrays: mixing curves of melt extraction trajectories?"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230853","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Site U1350"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230854","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Source of oceanic magnetic anomalies and the geomagnetic polarity timescale"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230855","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Site 306: Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230860","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Site 1213"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230976","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Constraining the rapid construction of TAMU Massif at an ~145Myr old triple junction, Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230978","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Leg 198 synthesis: a remarkable 120-m.y. record of climate and oceanography from Shatsky Rise, northwest Pacific Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230980","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Site U1348"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230983","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Correction of marine magnetic data to make a magnetic anomaly map for Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683230987","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The “plate” model for the genesis of melting anomalies"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231107","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Site U1346"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231108","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Boron and chlorine contents of basalts from the Shatsky Rise, IODP Expedition 324: Implications for the alteration of oceanic plateaus"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231113","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Shatsky Rise oceanic plateau structure from 2D multichannel seismic reflection profiles and implications for oceanic plateau formation"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231122","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Origin and evolution of magmas on the Ontong Java Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231235","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Ontong Java Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231238","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mesozoic magnetic anomalies, oceanic plateaus, and seamount chains in the northwestern Pacific Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231241","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Shatsky Rise: seismic stratigraphy and sedimentary record of Pacific paleoceanography since Early Cretaceous"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231248","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Noble gas evidence for the presence of recycled material in magma sources of Shatsky Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231364","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A hypothesis on terrestrial catastrophes: wedges of very thick oceanward-dipping layers beneath passive margins — their origin and paleoenvironmental significance"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231372","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Revised Pacific M-anomaly geomagnetic polarity timescale"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231374","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Hawaiian-Emperor Chain"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231375","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Experimental petrology of basement lavas from Ocean Drilling Program Leg192: implications for differentiation processes in Ontong Java Plateau magmas"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231489","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Divergence between paleomagnetic and hotspot-model-predicted polar wander for the Pacific plate with implications for hotspot fixity"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231491","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Recent MORB volcaniclastic explosive deposits formed between 500 and 1750m.b.s.l. on the axis of the Mid-Atlantic Ridge, south of the Azores"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231497","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional simulations of mantle convection with a thermo-chemical boundary layer: D”?"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231500","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Data report: High-resolution site survey seismic reflection data for ODP Leg 198 drilling on Shatsky Rise, northwest Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231503","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Paleomagnetism of igneous rocks from the Shatsky Rise: implications for paleolatitude and oceanic plateau volcanism"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231505","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Emplacement of continental flood basalt lava flows"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231620","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Leg 192 synthesis: Origin and evolution of the Ontong Java Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231621","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Data report: Si, Al, Fe, Ca, and K systematics of volcaniclastic sediments from selected cores of Hole U1347A, IODP Expedition 324"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231623","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Leg 192 summary"}]},{"@id":"https://cir.nii.ac.jp/crid/1371412891683231627","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Partial melting below the Ontong Java Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1373665080427497088","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Methods for resolving the origin of large igneous provinces from crustal seismology"}]},{"@id":"https://cir.nii.ac.jp/crid/1373665080427497089","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An empirical method for calculating melt compositions produced beneath mid-ocean ridges: application for axis and off-axis (seamounts) melting"}]},{"@id":"https://cir.nii.ac.jp/crid/1373665080427497090","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic tomography of Shatsky Rise by adaptive importance sampling"}]},{"@id":"https://cir.nii.ac.jp/crid/1373665080427497091","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Pacific absolute plate motion since 145Ma: An assessment of the fixed hotspot hypothesis"}]},{"@id":"https://cir.nii.ac.jp/crid/1373665080427497092","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mesozoic magnetic anomaly lineations and seafloor spreading history of the northwestern Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1373665080427497216","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"M-sequence geomagnetic polarity time scale (MHTC12) that steadies global spreading rates and incorporates astrochronology"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240892672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Results of Basement Drilling on Oceanic LIPs"},{"@language":"ja","@value":"巨大海台をつくる基盤溶岩の掘削成果"},{"@language":"ja-Kana","@value":"キョダイカイダイ オ ツクル キバン ヨウガン ノ クッサク セイカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390289475879746304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Testing the Ontong Java Nui Hypothesis: The Largest Supervolcano Ever on Earth"},{"@language":"ja","@value":"超オントンジャワ仮説の検証"},{"@value":"超オントンジャワ仮説の検証 : 地球最大の超巨大火山"},{"@language":"ja-Kana","@value":"チョウオントンジャワ カセツ ノ ケンショウ : チキュウ サイダイ ノ チョウキョダイ カザン"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792001112704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Near-ridge-axis volcanism affected by hotspot : insights from effective elastic thickness and topography of the Ojin Rise Seamounts, east of Shatsky Rise in the northwest Pacific Ocean"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.earscirev.2016.05.011"},{"@type":"KAKEN","@value":"PRODUCT-21034719"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-1140-5_references_DOI_7NHbL0Irnym5Bz4mjgJp4mJnDWA"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2020.105652_references_DOI_7NHbL0Irnym5Bz4mjgJp4mJnDWA"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00578-8_references_DOI_7NHbL0Irnym5Bz4mjgJp4mJnDWA"},{"@type":"CROSSREF","@value":"10.1029/2019jb019116_references_DOI_7NHbL0Irnym5Bz4mjgJp4mJnDWA"},{"@type":"CROSSREF","@value":"10.3389/feart.2022.994580_references_DOI_7NHbL0Irnym5Bz4mjgJp4mJnDWA"},{"@type":"CROSSREF","@value":"10.1080/00206814.2023.2224426_references_DOI_7NHbL0Irnym5Bz4mjgJp4mJnDWA"},{"@type":"CROSSREF","@value":"10.5026/jgeography.130.559_references_DOI_7NHbL0Irnym5Bz4mjgJp4mJnDWA"},{"@type":"CROSSREF","@value":"10.1038/s41561-019-0390-y_references_DOI_7NHbL0Irnym5Bz4mjgJp4mJnDWA"},{"@type":"CROSSREF","@value":"10.1130/b38019.1_references_DOI_7NHbL0Irnym5Bz4mjgJp4mJnDWA"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2016.0054_references_DOI_7NHbL0Irnym5Bz4mjgJp4mJnDWA"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2018.08.029_references_DOI_7NHbL0Irnym5Bz4mjgJp4mJnDWA"}]}