{"@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/1360011146070352000.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/90jb02416"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F90JB02416"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/90JB02416"}}],"dc:title":[{"@value":"Rapid inversion of two‐ and three‐dimensional magnetotelluric data"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We have developed an efficient iterative inversion method applicable to both two‐dimensional (2D) and three‐dimensional magnetotelluric data. The method approximates horizontal derivative terms with their values calculated from the fields of the previous iteration. The equations at each horizontal coordinate then become uncoupled. At each iteration this allows separate inversions for the improved conductivity profile beneath each measurement site. Resultant profiles are interpolated to form a new multidimensional model for which the fields for the next iteration are calculated. The method is extremely fast, and tests with 2D data show very promising results.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380011146070352001","@type":"Researcher","foaf:name":[{"@value":"J. Torquil Smith"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011146070352000","@type":"Researcher","foaf:name":[{"@value":"John R. Booker"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1991-03-10","prism:volume":"96","prism:number":"B3","prism:startingPage":"3905","prism:endingPage":"3922"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F90JB02416"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/90JB02416"}],"createdAt":"2008-02-06","modifiedAt":"2023-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360285710546317824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A regularized three-dimensional magnetotelluric inversion with a minimum gradient support constraint"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205196877568","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"インドネシア東部フローレス島パジャワ地熱地域におけるMT法データの2次元及び3次元解析"},{"@language":"en","@value":"2-D and 3-D interpretation of magnetotelluric data in the Bajawa geothermal field, central Flores, Indonesia"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206509150208","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geoelectric structure beneath limestones of the Sao Francisco Basin, Brazil"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512697472","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-dimensional inversion of static-shifted magnetotelluric data"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681485866752","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"2-D georesistivity structure in the central part of the northeastern Japan arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489980928","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Relation of the graphite and fluid bearing conducting dikes to the tectonics and seismicity"},{"@value":"Relation of the graphite and fluid bearing conducting dikes to the tectonics and seismicity (Review on the Transdanubian crustal conductivity anomaly)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681490087168","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Magnetotelluric soundings across the Taubaté Basin, Southeast Brazil"},{"@value":"Magnetotelluric soundings across the Taubate Basin, Southeast Brazil"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681490091392","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Analysis of magnetotelluric data along the Lithoprobe seismic line 21 in the Blake River Group, Abitibi, Canada"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681490258944","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Conductivity distribution and seismicity in the northeastern Japan Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367053035520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Regularized magnetotelluric inversion based on a minimum support gradient stabilizing functional"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/90jb02416"},{"@type":"CROSSREF","@value":"10.1186/bf03353051_references_DOI_EUMe9lXN9S0pQ9zmPSxM5awe5FM"},{"@type":"CROSSREF","@value":"10.1186/bf03353406_references_DOI_EUMe9lXN9S0pQ9zmPSxM5awe5FM"},{"@type":"CROSSREF","@value":"10.1186/bf03351578_references_DOI_EUMe9lXN9S0pQ9zmPSxM5awe5FM"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0743-y_references_DOI_EUMe9lXN9S0pQ9zmPSxM5awe5FM"},{"@type":"CROSSREF","@value":"10.1111/j.1365-246x.2012.05379.x_references_DOI_EUMe9lXN9S0pQ9zmPSxM5awe5FM"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.53.265_references_DOI_EUMe9lXN9S0pQ9zmPSxM5awe5FM"},{"@type":"CROSSREF","@value":"10.1186/bf03351687_references_DOI_EUMe9lXN9S0pQ9zmPSxM5awe5FM"},{"@type":"CROSSREF","@value":"10.1186/bf03353050_references_DOI_EUMe9lXN9S0pQ9zmPSxM5awe5FM"},{"@type":"CROSSREF","@value":"10.1186/bf03351577_references_DOI_EUMe9lXN9S0pQ9zmPSxM5awe5FM"},{"@type":"CROSSREF","@value":"10.1186/bf03353046_references_DOI_EUMe9lXN9S0pQ9zmPSxM5awe5FM"}]}