{"@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/1363670320066064512.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1190/1.1444745"}},{"identifier":{"@type":"URI","@value":"https://pubs.geoscienceworld.org/seg/geophysics/article-pdf/65/2/512/3685130/gsgpy_65_2_512.pdf"}}],"dc:title":[{"@value":"Euler deconvolution of gravity tensor gradient data"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n                  <jats:p>Tensor Euler deconvolution has been developed to help interpret gravity tensor gradient data in terms of 3-D subsurface geological structure. Two forms of Euler deconvolution have been used in this study: conventional Euler deconvolution using three gradients of the vertical component of the gravity vector and tensor Euler deconvolution using all tensor gradients.</jats:p>\n                  <jats:p>These methods have been tested on point, prism, and cylindrical mass models using line and gridded data forms. The methods were then applied to measured gravity tensor gradient data for the Eugene Island area of the Gulf of Mexico using gridded and ungridded data forms. The results from the model and measured data show significantly improved performance of the tensor Euler deconvolution method, which exploits all measured tensor gradients and hence provides additional constraints on the Euler solutions.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320066064385","@type":"Researcher","foaf:name":[{"@value":"Changyou Zhang"}],"jpcoar:affiliationName":[{"@value":"∗Formerly Univ. of Leeds, School of Earth Sciences, Leeds LS2 9JT, UK; presently 117-401 Westview St., Coquitlam, British Columbia V3K 3W3, Canada."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320066064387","@type":"Researcher","foaf:name":[{"@value":"Martin F. Mushayandebvu"}],"jpcoar:affiliationName":[{"@value":"‡Univ. of Leeds, School of Earth Sciences, Leeds LS2 9JT, UK. E-mail: mushaya@earth.leeds.ac.uk."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320066064512","@type":"Researcher","foaf:name":[{"@value":"Alan B. Reid"}],"jpcoar:affiliationName":[{"@value":"∗∗Formerly GETECH, c/o Univ. of Leeds, School of Earth Sciences, Leeds; presently Reid Geophysics, 49 Carr Bridge Dr., Leeds LS16 7LB, UK. E-mail: alan@reidgeophys.freeserve.co.uk."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320066064386","@type":"Researcher","foaf:name":[{"@value":"J. Derek Fairhead"}],"jpcoar:affiliationName":[{"@value":"§GETECH, Univ. of Leeds, c/o School of Earth Sciences, Leeds LS2 9JT, UK. E-mail: jdf@getech.leeds.ac.uk."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320066064384","@type":"Researcher","foaf:name":[{"@value":"Mark E. Odegard"}],"jpcoar:affiliationName":[{"@value":"††Formerly Unocal Corp. E&P Technology, USA, Sugar Land, Texas; presently GETECH Inc., 12946 Dairy Ashford Rd., Suite 250, Sugar Land, Texas 77478. E-mail: meo@getech.com."}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"19422156"},{"@type":"PISSN","@value":"00168033"}],"prism:publicationName":[{"@value":"Geophysics"}],"dc:publisher":[{"@value":"Society of Exploration Geophysicists"}],"prism:publicationDate":"1999-10-20","prism:volume":"65","prism:number":"2","prism:startingPage":"512","prism:endingPage":"520"},"reviewed":"false","url":[{"@id":"https://pubs.geoscienceworld.org/seg/geophysics/article-pdf/65/2/512/3685130/gsgpy_65_2_512.pdf"}],"createdAt":"2002-10-11","modifiedAt":"2025-12-11","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360848665278689920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Inconsistent Structure and Motion of the Eastern Median Tectonic Line, Southwest Japan, during the Quaternary"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681471822848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"重力勾配テンソルの固有ベクトルを用いた断層あるいは構造境界の傾斜角の推定"},{"@language":"en","@value":"Estimation of dip angle of fault or structural boundary by eigenvectors of gravity gradient tensors"},{"@language":"ja-Kana","@value":"ジュウリョク コウバイ テンソル ノ コユウ ベクトル オ モチイタ ダンソウ アルイハ コウゾウ キョウカイ ノ ケイシャカク ノ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681471852032","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"重力勾配テンソルを用いた構造境界抽出のための半自動解釈手法"},{"@language":"en","@value":"Semi-automatic interpretation methods for extracting structural boundaries using gravity gradient tensors"},{"@language":"ja-Kana","@value":"ジュウリョク コウバイ テンソル オ モチイタ コウゾウ キョウカイ チュウシュツ ノ タメ ノ ハンジドウ カイシャク シュホウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681474013824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"重力偏差テンソルのg<sub>zz</sub>成分のパワースペクトルと平均境界層深度の関係"},{"@language":"en","@value":"Relationship between the average depth of a stratum boundary and the power spectrum of the g<sub>zz</sub> component of a gravity gradient tensor"},{"@value":"重力偏差テンソルのgzz成分のパワースペクトルと平均境界層深度の関係"},{"@language":"ja-Kana","@value":"ジュウリョク ヘンサ テンソル ノ gzz セイブン ノ パワースペクトル ト ヘイキン キョウカイソウ シンド ノ カンケイ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588891962970624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Eigenvector of gravity gradient tensor for estimating fault dips considering fault type"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1190/1.1444745"},{"@type":"CROSSREF","@value":"10.1186/s40645-017-0130-0_references_DOI_Quovs0e8RQJbAA49Mk7o2A5WSoe"},{"@type":"CROSSREF","@value":"10.3124/segj.70.1_references_DOI_Quovs0e8RQJbAA49Mk7o2A5WSoe"},{"@type":"CROSSREF","@value":"10.3124/segj.68.277_references_DOI_Quovs0e8RQJbAA49Mk7o2A5WSoe"},{"@type":"CROSSREF","@value":"10.5772/67964_references_DOI_Quovs0e8RQJbAA49Mk7o2A5WSoe"},{"@type":"CROSSREF","@value":"10.3124/segj.69.53_references_DOI_Quovs0e8RQJbAA49Mk7o2A5WSoe"}]}