{"@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/1360004229805970176.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2016gl071331"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016GL071331"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL071331"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Electromagnetic evidence for volatile‐rich upwelling beneath the society hotspot, French Polynesia"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>We have conducted a seafloor magnetotelluric survey that images, for the first time, three‐dimensional electrical conductivity structure in the upper mantle beneath the Society hotspot. A striking feature in our model is a high‐conductivity anomaly a few hundred kilometers in diameter, which is continuous from the lowest part of the upper mantle to a depth of approximately 50 km below sea level. Using theoretical and experimental results from mineral physics, we interpret the high‐conductivity anomaly as evidence of the melt fraction up to 2.2 vol.%, which is robust regardless of assumed temperature, and the existence of carbonated silicate melt beneath the hotspot. Our results suggest that the Society hotspot is a pathway for ascending volatiles from the deeper part of the upper mantle to the surface.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420564276158643968","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"00509713"},{"@type":"NRID","@value":"1000000509713"},{"@type":"NRID","@value":"9000019187011"},{"@type":"NRID","@value":"9000380980841"},{"@type":"NRID","@value":"9000019191846"},{"@type":"NRID","@value":"9000248238787"},{"@type":"NRID","@value":"9000369737039"},{"@type":"NRID","@value":"9000389433957"},{"@type":"NRID","@value":"9000398137202"},{"@type":"NRID","@value":"9000257986308"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/noriko_t"}],"foaf:name":[{"@value":"Noriko Tada"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine‐Earth Science and Technology  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805970193","@type":"Researcher","foaf:name":[{"@value":"Pascal Tarits"}],"jpcoar:affiliationName":[{"@value":"UMR‐Domaines Océaniques Institut Universitaire Européen de la Mer  Plouzane France"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801189433856","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"70371721"},{"@type":"NRID","@value":"1000070371721"},{"@type":"NRID","@value":"9000014234770"},{"@type":"NRID","@value":"9000022033670"},{"@type":"NRID","@value":"9000009002889"},{"@type":"NRID","@value":"9000018767740"},{"@type":"NRID","@value":"9000001756168"},{"@type":"NRID","@value":"9000254741255"},{"@type":"NRID","@value":"9000019191847"},{"@type":"NRID","@value":"9000248238788"},{"@type":"NRID","@value":"9000291608041"},{"@type":"NRID","@value":"9000414373333"},{"@type":"NRID","@value":"9000369737038"},{"@type":"NRID","@value":"9000389433960"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/KiyoshiBaba"}],"foaf:name":[{"@value":"Kiyoshi Baba"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420564276176837504","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"70134632"},{"@type":"NRID","@value":"1000070134632"},{"@type":"NRID","@value":"9000253256398"},{"@type":"NRID","@value":"9000014234017"},{"@type":"NRID","@value":"9000003141466"},{"@type":"NRID","@value":"9000254739534"},{"@type":"NRID","@value":"9000000519303"},{"@type":"NRID","@value":"9000253255986"},{"@type":"NRID","@value":"9000004600174"},{"@type":"NRID","@value":"9000293528242"},{"@type":"NRID","@value":"9000253256368"},{"@type":"NRID","@value":"9000001756170"},{"@type":"NRID","@value":"9000254261928"},{"@type":"NRID","@value":"9000254741257"},{"@type":"NRID","@value":"9000253258010"},{"@type":"NRID","@value":"9000252829732"},{"@type":"NRID","@value":"9000016923551"},{"@type":"NRID","@value":"9000351087859"},{"@type":"NRID","@value":"9000256136458"},{"@type":"NRID","@value":"9000020466249"},{"@type":"NRID","@value":"9000020306524"},{"@type":"NRID","@value":"9000399010625"},{"@type":"NRID","@value":"9000254753828"},{"@type":"NRID","@value":"9000253255400"},{"@type":"NRID","@value":"9000380425076"},{"@type":"NRID","@value":"9000248238791"},{"@type":"NRID","@value":"9000009170741"},{"@type":"NRID","@value":"9000361320084"},{"@type":"NRID","@value":"9000253255265"},{"@type":"NRID","@value":"9000291607663"},{"@type":"NRID","@value":"9000369737048"},{"@type":"NRID","@value":"9000389433954"},{"@type":"NRID","@value":"9000000143973"},{"@type":"NRID","@value":"9000254740094"},{"@type":"NRID","@value":"9000267797219"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0046404"}],"foaf:name":[{"@value":"Hisashi Utada"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805970054","@type":"Researcher","foaf:name":[{"@value":"Takafumi Kasaya"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine‐Earth Science and Technology  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1030003658520002433","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"20359178"},{"@type":"NRID","@value":"1000020359178"},{"@type":"NRID","@value":"9000258406871"},{"@type":"NRID","@value":"9000007275010"},{"@type":"NRID","@value":"9000391404986"},{"@type":"NRID","@value":"9000007278762"},{"@type":"NRID","@value":"9000010714552"},{"@type":"NRID","@value":"9000002846380"},{"@type":"NRID","@value":"9000019128635"},{"@type":"NRID","@value":"9000002496494"},{"@type":"NRID","@value":"9000391402251"},{"@type":"NRID","@value":"9000256074113"},{"@type":"NRID","@value":"9000018811597"},{"@type":"NRID","@value":"9000391402499"},{"@type":"NRID","@value":"9000370254130"},{"@type":"NRID","@value":"9000370254140"},{"@type":"NRID","@value":"9000283905545"}],"foaf:name":[{"@value":"Daisuke Suetsugu"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine‐Earth Science and Technology  Yokosuka Japan"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1890020693266532097","@type":"Researcher","foaf:name":[{"@value":"Domaines Océaniques (LDO) ; Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1890020693266532102","@type":"Researcher","foaf:name":[{"@value":"Institut Universitaire Européen de la Mer (IUEM) ; Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916127677700","@type":"Researcher","foaf:name":[{"@value":"POTHIER, Nathalie"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916127677699","@type":"Researcher","foaf:name":[{"@value":"Domaines Océaniques (LDO)"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916127677697","@type":"Researcher","foaf:name":[{"@value":"Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916127677696","@type":"Researcher","foaf:name":[{"@value":"Institut Universitaire Européen de la Mer (IUEM)"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916127677698","@type":"Researcher","foaf:name":[{"@value":"Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)"}]}],"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":"2016-12-03","prism:volume":"43","prism:number":"23","prism:startingPage":"12021","prism:endingPage":"12026"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016GL071331"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL071331"}],"createdAt":"2016-11-19","modifiedAt":"2023-09-09","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=three-dimensional%20inversion","dc:title":"three-dimensional inversion"},{"@id":"https://cir.nii.ac.jp/all?q=550","dc:title":"550"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.STU%5DSciences%20of%20the%20Universe%20%5Bphysics%5D/Earth%20Sciences","dc:title":"[SDU.STU]Sciences of the Universe [physics]/Earth Sciences"},{"@id":"https://cir.nii.ac.jp/all?q=partial%20melt","dc:title":"partial melt"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU%5D%20Sciences%20of%20the%20Universe%20%5Bphysics%5D","dc:title":"[SDU] Sciences of the Universe [physics]"},{"@id":"https://cir.nii.ac.jp/all?q=volatiles","dc:title":"volatiles"},{"@id":"https://cir.nii.ac.jp/all?q=marine%20magnetotellurics","dc:title":"marine magnetotellurics"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU%5DSciences%20of%20the%20Universe%20%5Bphysics%5D","dc:title":"[SDU]Sciences of the Universe [physics]"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.STU%5D%20Sciences%20of%20the%20Universe%20%5Bphysics%5D/Earth%20Sciences","dc:title":"[SDU.STU] Sciences of the Universe [physics]/Earth Sciences"},{"@id":"https://cir.nii.ac.jp/all?q=hotspot","dc:title":"hotspot"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781902844800","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H06475"},{"@type":"JGN","@value":"JP16H06475"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-16H06475/"}],"notation":[{"@language":"ja","@value":"スロー地震発生領域周辺の地震学的・電磁気学的構造の解明"},{"@language":"en","@value":"Study on Seismic and Electromagnetic Subsurface Structure around the Source of Slow Earthquakes"}]},{"@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/1040282256821599872","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15K05262"},{"@type":"JGN","@value":"JP15K05262"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15K05262/"}],"notation":[{"@language":"ja","@value":"海底電磁気観測網を生かしたマントル遷移層内水分布イメージングの革新"},{"@language":"en","@value":"Inovation for the imaging of water in the mantle transition zone using seafloor electromagnetic array data"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338305284992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Marine magnetotelluric inversion with an unstructured tetrahedral mesh"}]},{"@id":"https://cir.nii.ac.jp/crid/1050583402767207168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"TIARES Project -Tomographic investigation by seafloor array experiment for the Society hotspot"},{"@value":"TIARES Project—Tomographic investigation by seafloor array experiment for the Society hotspot"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004234589649792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Practical incorporation of local and regional topography in three-dimensional inversion of deep ocean magnetotelluric data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144203983744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geodynamics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168773594880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hydrothermal and Magmatic System of a Volcanic Island Inferred From Magnetotellurics, Seismicity, Self‐potential, and Thermal Image: An Example of Miyakejima (Japan)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691684285312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"South Pacific mantle plumes imaged by seismic observation on islands and seafloor"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617909532032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"New, improved version of generic mapping tools released"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619268615296","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Does partial melting explain geophysical anomalies?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094461449472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Partial melt in the oceanic low velocity zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584339755321472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Adjoint-based data assimilation for reconstruction of thermal convection in a highly viscous fluid from surface velocity and temperature snapshots"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570352641152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Electrical Structure in Marine Tectonic Settings"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044103632384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Variational Approach to the Theory of the Effective Magnetic Permeability of Multiphase Materials"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995022193024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The H/C ratios of Earth's near-surface and deep reservoirs, and consequences for deep Earth volatile cycles"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469972233856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Extent of the South Pacific Superswell"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944323210496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hydrogen partition coefficients between nominally anhydrous minerals and basaltic melts"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945227719936","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Degassing of CO2 and H2O in submarine lavas from the Society hotspot"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945757527552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"South Pacific hotspot swells dynamically supported by mantle flows"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893999690752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetotelluric imaging of the Society Islands hotspot"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845617715456","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Linear volcanism in French Polynesia"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319729082752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Electrical conductivity during incipient melting in the oceanic low-velocity zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794172989184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Correction of seafloor magnetotelluric data for topographic effects during inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794210077184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Bounded influence magnetotelluric response function estimation"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270733088768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Toward a unified hydrous olivine electrical conductivity law"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205317465600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The OJP array: seismological and electromagnetic observation on seafloor and islands in the Ontong Java Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1390859447985304960","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Thermochemical state of the oceanic lithosphere constrained from oceanic mantle peridotites"},{"@language":"ja","@value":"海洋マントルカンラン岩から探る海洋リソスフェアの熱化学状態"}]},{"@id":"https://cir.nii.ac.jp/crid/1574231876079631744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Electrical conductivity imaging of the Philippine Sea upper mantle using seafloor magnetotelluric data"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417161653504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Approximate treatment of seafloor topographic effects in three-dimensional marine magnetotelluric inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842051751936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Validity of the dispersion relations in magnetotellurics. Part II : synthetic and field data"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842060085504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Drift of an ocean bottom electromagnetometer from the Bonin to Ryukyu Islands : estimation of the path and travel time by numerical tracking experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842099392384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Upper mantle structure beneath the Society hotspot and surrounding region using broadband data from ocean floor and islands"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2016gl071331"},{"@type":"KAKEN","@value":"PRODUCT-21565991"},{"@type":"KAKEN","@value":"PRODUCT-20822449"},{"@type":"KAKEN","@value":"PRODUCT-21165240"},{"@type":"OPENAIRE","@value":"doi_dedup___::3f73bd87ac75d3ac57a78aff6c512f3e"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01273-4_references_DOI_Ucw6LMoIvoiJWlBh5ow6CLwLYrx"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01552-8_references_DOI_MJZQEfvYQ2M5gI3NsYkonc7ksbo"},{"@type":"CROSSREF","@value":"10.1029/2021jb022034_references_DOI_Ucw6LMoIvoiJWlBh5ow6CLwLYrx"},{"@type":"CROSSREF","@value":"10.2465/gkk.230204_references_DOI_Ucw6LMoIvoiJWlBh5ow6CLwLYrx"},{"@type":"CROSSREF","@value":"10.1093/gji/ggy171_references_DOI_Ucw6LMoIvoiJWlBh5ow6CLwLYrx"},{"@type":"CROSSREF","@value":"10.5918/jamstecr.26.54_references_DOI_Ucw6LMoIvoiJWlBh5ow6CLwLYrx"},{"@type":"CROSSREF","@value":"10.1093/gji/ggad417_references_DOI_Ucw6LMoIvoiJWlBh5ow6CLwLYrx"}]}