{"@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/1363670321336031232.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2011gl050177"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011GL050177"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2011GL050177"}}],"dc:title":[{"@value":"Magnetotelluric imaging of upper‐crustal convection plumes beneath the Taupo Volcanic Zone, New Zealand"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Broadband MT (magnetotelluric) data were recorded that form an array of measurements at the south‐eastern margin of the TVZ (Taupo Volcanic Zone), in the central North Island of New Zealand. These array data are used to investigate mechanisms by which the TVZ's extraordinarily high heat flux is transported to the surface. Taken together with seismological data, these MT data show compelling evidence that support a model of hydrothermal convection within the brittle (upper ∼6–7 km) part of the crust. Both 2‐D and 3‐D inversion models of these MT data show vertical low‐resistivity zones that connect surface geothermal fields to an inferred magmatic heat source that lies below the brittle‐ductile transition.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004236853259394","@type":"Researcher","foaf:name":[{"@value":"E. A. Bertrand"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670321336031232","@type":"Researcher","foaf:name":[{"@value":"T. G. Caldwell"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670321336031105","@type":"Researcher","foaf:name":[{"@value":"G. J. Hill"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670321336031239","@type":"Researcher","foaf:name":[{"@value":"E. L. Wallin"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670321336031234","@type":"Researcher","foaf:name":[{"@value":"S. L. Bennie"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670321336031238","@type":"Researcher","foaf:name":[{"@value":"N. Cozens"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670321336031233","@type":"Researcher","foaf:name":[{"@value":"S. A. Onacha"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670321336031237","@type":"Researcher","foaf:name":[{"@value":"G. A. Ryan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670321336031236","@type":"Researcher","foaf:name":[{"@value":"C. Walter"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670321336031104","@type":"Researcher","foaf:name":[{"@value":"A. Zaino"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670321336031235","@type":"Researcher","foaf:name":[{"@value":"P. Wameyo"}]}],"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":"2012-01","prism:volume":"39","prism:number":"2","prism:startingPage":"L02304"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011GL050177"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2011GL050177"}],"createdAt":"2011-12-28","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/1050573243559206016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimation of spatial distribution and fluid fraction of a potential supercritical geothermal reservoir by magnetotelluric data: a case study from Yuzawa geothermal field, NE Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050587981431089408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal magma pathway beneath Aso caldera inferred from three-dimensional electrical resistivity structure"},{"@value":"Crustal magma pathway beneath Aso caldera inferred from three‐dimensional electrical resistivity structure"},{"@value":"Crustal magma pathway beneath Aso caldera inferred from 3-D electrical resistivity structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183245608320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three‐Dimensional Electrical Resistivity Modeling to Elucidate the Crustal Magma Supply System Beneath Aso Caldera, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892090759936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magnetotelluric transect of Unzen graben, Japan : conductors associated with normal faults"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367119613824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Preparatory and precursory processes leading up to the 2014 phreatic eruption of Mount Ontake, Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2011gl050177"},{"@type":"CROSSREF","@value":"10.1002/2013jb010682_references_DOI_I3ldYnffcOq0D1IRBr3F2yxd7JB"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1004-z_references_DOI_EytDsMMHY9cNaj5X60fKyVpZmtK"},{"@type":"CROSSREF","@value":"10.1029/2018jb015951_references_DOI_I3ldYnffcOq0D1IRBr3F2yxd7JB"},{"@type":"CROSSREF","@value":"10.1029/2021jb022911_references_DOI_I3ldYnffcOq0D1IRBr3F2yxd7JB"},{"@type":"CROSSREF","@value":"10.1186/s40623-015-0288-x_references_DOI_I3ldYnffcOq0D1IRBr3F2yxd7JB"},{"@type":"CROSSREF","@value":"10.1002/2016gl070315_references_DOI_I3ldYnffcOq0D1IRBr3F2yxd7JB"}]}