{"@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/1362825895879964672.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1190/1.3026538"}},{"identifier":{"@type":"URI","@value":"https://pubs.geoscienceworld.org/seg/geophysics/article-pdf/74/1/L7/3214868/gsgpy_74_1_L7.pdf"}}],"dc:title":[{"@value":"3D magnetic data-space inversion with sparseness constraints"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n                  <jats:p>I have developed an inversion approach that determines a 3D susceptibility distribution that produces a given magnetic anomaly. The subsurface model consists of a 3D, equally spaced array of dipoles. The inversion incorporates a model norm that enforces sparseness and depth weighting of the solution. Sparseness is imposed by using the Cauchy norm on model parameters. The inverse problem is posed in the data space, leading to a linear system of equations with dimensions based on the number of data, N. This contrasts with the standard least-squares solution, derived through operations within the M-dimensional model space (M being the number of model parameters). Hence, the data-space method combined with a conjugate gradient algorithm leads to computational efficiency by dealing with an N×N system versus an M×M one, where N≪M. Tests on synthetic data show that sparse inversion produces a much more focused solution compared with a standard model-space, least-squares inversion. The inversion of aeromagnetic data collected over a Precambrian Shield area again shows that including the sparseness constraint leads to a simpler and better resolved solution. The degree of improvement in model resolution for the sparse case is quantified using the resolution matrix.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825895879964544","@type":"Researcher","foaf:name":[{"@value":"Mark Pilkington"}],"jpcoar:affiliationName":[{"@value":"1Geological Survey of Canada, Ottawa, Ontario, Canada. E-mail: mpilking@nrcan.gc.ca."}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"19422156"},{"@type":"PISSN","@value":"00168033"}],"prism:publicationName":[{"@value":"Geophysics"}],"dc:publisher":[{"@value":"Society of Exploration Geophysicists"}],"prism:publicationDate":"2008-12-12","prism:volume":"74","prism:number":"1","prism:startingPage":"L7","prism:endingPage":"L15"},"reviewed":"false","url":[{"@id":"https://pubs.geoscienceworld.org/seg/geophysics/article-pdf/74/1/L7/3214868/gsgpy_74_1_L7.pdf"}],"createdAt":"2008-12-12","modifiedAt":"2025-12-11","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050845763318233472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"3-D inversion of magnetic data based on the L1-L2 norm regularization"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168799766656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magnetic inversion to recover the subsurface block structures based on<i>L</i>1 norm and total variation regularization"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306906091106944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"An efficient decoupled 3-D axial anisotropic resistivity inversion for magnetotelluric data with OpenMP parallelization"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1190/1.3026538"},{"@type":"CROSSREF","@value":"10.1093/gji/ggab355_references_DOI_N9ZuPZG35thn9RfIrcGVtuiUXbS"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-02113-5_references_DOI_N9ZuPZG35thn9RfIrcGVtuiUXbS"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1052-4_references_DOI_N9ZuPZG35thn9RfIrcGVtuiUXbS"}]}