{"@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/1361418520200670592.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2010gl043110"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2010GL043110"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2010GL043110"}}],"dc:title":[{"@value":"Three‐dimensional electrical resistivity image of magma beneath an active continental rift, Taupo Volcanic Zone, New Zealand"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Magmatic activity in regions of continental extension may result in huge (>400 km<jats:sup>3</jats:sup>) explosive eruptions of viscous, gas‐rich silicic‐magma. Geochemical and geological data suggest that the large volumes of magma erupted are produced by extracting interstitial liquid from a long‐lived ‘mush zone’ (a mixture of solid crystals and liquid melt) that accumulates in liquid‐dominated lenses at the top of a much thicker region of lower melt‐fraction mush. Such lenses will be highly electrically conductive compared with normal mid‐crustal rocks. Here we use results of 220 magnetotelluric (MT) soundings to construct a 3‐D electrical resistivity image of the northern (silicic) part of New Zealand's Taupo Volcanic Zone, a young continental rift associated with very high heat flow and intense silicic volcanism. The electrical resistivity image shows a plume‐like structure of high conductivity, interpreted to be a zone of interconnected melt, rising from depths >35 km beneath the axis of extension.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381418520200670593","@type":"Researcher","foaf:name":[{"@value":"Wiebke Heise"}],"jpcoar:affiliationName":[{"@value":"GNS Science  Lower Hutt New Zealand"},{"@value":"CGUL, IDL, Faculdade de Ciências Universidade de Lisboa  Lisbon Portugal"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520200670595","@type":"Researcher","foaf:name":[{"@value":"T. Grant Caldwell"}],"jpcoar:affiliationName":[{"@value":"GNS Science  Lower Hutt New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520200670592","@type":"Researcher","foaf:name":[{"@value":"Hugh M. Bibby"}],"jpcoar:affiliationName":[{"@value":"GNS Science  Lower Hutt New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520200670594","@type":"Researcher","foaf:name":[{"@value":"Stewart L. Bennie"}],"jpcoar:affiliationName":[{"@value":"GNS Science  Lower Hutt New Zealand"}]}],"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":"2010-05","prism:volume":"37","prism:number":"10","prism:startingPage":"L10301"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2010GL043110"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2010GL043110"}],"createdAt":"2010-05-17","modifiedAt":"2023-10-30","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338420421248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional resistivity structure and magma plumbing system of the Kirishima volcanoes as inferred from broad-band magnetotelluric data"}]},{"@id":"https://cir.nii.ac.jp/crid/1050869456405311104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Magmatic–hydrothermal system of Aso Volcano, Japan, inferred from electrical resistivity structures"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298345525014656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magmatic fluid pathways in the upper crust: insights from dense magnetotelluric observations around the Kuju Volcanoes, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118683406336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Inter- and intra-crystal quartz δ18O homogeneity at Okataina volcano, Aotearoa New Zealand: Implications for rhyolite genesis"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206525416448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地殻・上部マントルの電気比抵抗構造：観測の原理・精度と物性データの現状"},{"@language":"en","@value":"An overview of electrical resistivity in the crust and upper mantle: principle of magnetotelluric method, accuracy and resolution of resistivity modeling, and electrical resistivity feature of crustal and mantle rocks and minerals"},{"@language":"ja-Kana","@value":"チカク ジョウブ マントル ノ デンキヒ テイコウ コウゾウ カンソク ノ ゲンリ セイド ト ブッセイ データ ノ ゲンジョウ"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2010gl043110"},{"@type":"CROSSREF","@value":"10.1002/2013jb010682_references_DOI_WBpHIQ2VetOgq5G96kRyyV169KE"},{"@type":"CROSSREF","@value":"10.2465/gkk.110131b_references_DOI_WBpHIQ2VetOgq5G96kRyyV169KE"},{"@type":"CROSSREF","@value":"10.1093/gji/ggab368_references_DOI_WBpHIQ2VetOgq5G96kRyyV169KE"},{"@type":"CROSSREF","@value":"10.1016/j.jvolgeores.2021.107430_references_DOI_WBpHIQ2VetOgq5G96kRyyV169KE"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01180-8_references_DOI_WBpHIQ2VetOgq5G96kRyyV169KE"}]}