{"@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/1360306906091106944.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1186/s40623-024-02113-5"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1186/s40623-024-02113-5.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1186/s40623-024-02113-5/fulltext.html"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"An efficient decoupled 3-D axial anisotropic resistivity inversion for magnetotelluric data with OpenMP parallelization"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n          <jats:p>We have developed two novel axial anisotropic inversion codes for magnetotelluric (MT) data: a full axial inversion and a decoupled axial inversion. Both codes are based on the data space Gauss–Newton inversion method used in the WSINV3DMT code, enhanced with OpenMP parallelization and Intel MKL PARDISO direct solver for improved computational efficiency. The full axial inversion searches for three axial anisotropic resistivity elements <jats:inline-formula>\n              <jats:alternatives>\n                <jats:tex-math>$${\\rho }_{xx}$$</jats:tex-math>\n                <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\">\n                  <mml:msub>\n                    <mml:mi>ρ</mml:mi>\n                    <mml:mrow>\n                      <mml:mi>xx</mml:mi>\n                    </mml:mrow>\n                  </mml:msub>\n                </mml:math>\n              </jats:alternatives>\n            </jats:inline-formula>, <jats:inline-formula>\n              <jats:alternatives>\n                <jats:tex-math>$${\\rho }_{yy}$$</jats:tex-math>\n                <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\">\n                  <mml:msub>\n                    <mml:mi>ρ</mml:mi>\n                    <mml:mrow>\n                      <mml:mi>yy</mml:mi>\n                    </mml:mrow>\n                  </mml:msub>\n                </mml:math>\n              </jats:alternatives>\n            </jats:inline-formula>, and <jats:inline-formula>\n              <jats:alternatives>\n                <jats:tex-math>$${\\rho }_{zz}$$</jats:tex-math>\n                <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\">\n                  <mml:msub>\n                    <mml:mi>ρ</mml:mi>\n                    <mml:mrow>\n                      <mml:mi>zz</mml:mi>\n                    </mml:mrow>\n                  </mml:msub>\n                </mml:math>\n              </jats:alternatives>\n            </jats:inline-formula>. Based on our prior influence studies, we identified contrasting influence patterns: <jats:inline-formula>\n              <jats:alternatives>\n                <jats:tex-math>$${\\rho }_{xx}$$</jats:tex-math>\n                <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\">\n                  <mml:msub>\n                    <mml:mi>ρ</mml:mi>\n                    <mml:mrow>\n                      <mml:mi>xx</mml:mi>\n                    </mml:mrow>\n                  </mml:msub>\n                </mml:math>\n              </jats:alternatives>\n            </jats:inline-formula> has a strong influence on <jats:italic>Z</jats:italic>\n            <jats:sub>\n              <jats:italic>xy</jats:italic>\n            </jats:sub> and <jats:italic>Z</jats:italic>\n            <jats:sub>\n              <jats:italic>yy</jats:italic>\n            </jats:sub>, whereas <jats:inline-formula>\n              <jats:alternatives>\n                <jats:tex-math>$${\\rho }_{yy}$$</jats:tex-math>\n                <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\">\n                  <mml:msub>\n                    <mml:mi>ρ</mml:mi>\n                    <mml:mrow>\n                      <mml:mi>yy</mml:mi>\n                    </mml:mrow>\n                  </mml:msub>\n                </mml:math>\n              </jats:alternatives>\n            </jats:inline-formula> has a strong influence on <jats:italic>Z</jats:italic>\n            <jats:sub>\n              <jats:italic>yx</jats:italic>\n            </jats:sub> and <jats:italic>Z</jats:italic>\n            <jats:sub>\n              <jats:italic>xx</jats:italic>\n            </jats:sub>, while <jats:inline-formula>\n              <jats:alternatives>\n                <jats:tex-math>$${\\rho }_{zz}$$</jats:tex-math>\n                <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\">\n                  <mml:msub>\n                    <mml:mi>ρ</mml:mi>\n                    <mml:mrow>\n                      <mml:mi>zz</mml:mi>\n                    </mml:mrow>\n                  </mml:msub>\n                </mml:math>\n              </jats:alternatives>\n            </jats:inline-formula> has negligible impact on all responses. We, therefore, proposed a decoupled axial inversion. This novel technique splits the full axial inversion into two independent modes: <jats:inline-formula>\n              <jats:alternatives>\n                <jats:tex-math>$${\\rho }_{xx}$$</jats:tex-math>\n                <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\">\n                  <mml:msub>\n                    <mml:mi>ρ</mml:mi>\n                    <mml:mrow>\n                      <mml:mi>xx</mml:mi>\n                    </mml:mrow>\n                  </mml:msub>\n                </mml:math>\n              </jats:alternatives>\n            </jats:inline-formula>- and <jats:inline-formula>\n              <jats:alternatives>\n                <jats:tex-math>$${\\rho }_{yy}$$</jats:tex-math>\n                <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\">\n                  <mml ..."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380306906091106974","@type":"Researcher","foaf:name":[{"@value":"Wisart Thongyoy"}]},{"@id":"https://cir.nii.ac.jp/crid/1380306906091106833","@type":"Researcher","foaf:name":[{"@value":"Weerachai Siripunvaraporn"}]},{"@id":"https://cir.nii.ac.jp/crid/1380306906091106837","@type":"Researcher","foaf:name":[{"@value":"Puwis Amatayakul"}]},{"@id":"https://cir.nii.ac.jp/crid/1380306906091106963","@type":"Researcher","foaf:name":[{"@value":"Tawat Rung-Arunwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380306906091106980","@type":"Researcher","foaf:name":[{"@value":"Kiyoshi Baba"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18805981"}],"prism:publicationName":[{"@value":"Earth, Planets and Space"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2025-01-23","prism:volume":"77","prism:number":"1"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://creativecommons.org/licenses/by/4.0","https://creativecommons.org/licenses/by/4.0"],"url":[{"@id":"https://link.springer.com/content/pdf/10.1186/s40623-024-02113-5.pdf"},{"@id":"https://link.springer.com/article/10.1186/s40623-024-02113-5/fulltext.html"}],"createdAt":"2025-01-23","modifiedAt":"2025-01-23","project":[{"@id":"https://cir.nii.ac.jp/crid/1040295802078230144","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23H00138"},{"@type":"JGN","@value":"JP23H00138"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23H00138/"}],"notation":[{"@language":"ja","@value":"海洋アセノスフェアの粘性率を制約するための海底物理観測・モデリング国際協働研究"},{"@language":"en","@value":"International collaborative research on the viscosity of the oceanic asthenosphere through marine geophysical observations and geodynamic modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1040299826878739456","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23K22601"},{"@type":"JGN","@value":"JP23K22601"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23K22601/"}],"notation":[{"@language":"ja","@value":"プレート成長標準モデル：プレートテクトニクスからプレートダイナミクスへ"}]},{"@id":"https://cir.nii.ac.jp/crid/1040581301854573696","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23K20893"},{"@type":"JGN","@value":"JP23K20893"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23K20893/"}],"notation":[{"@language":"ja","@value":"マントル遷移層探査のための海底観測技術の高度化"},{"@language":"en","@value":"Advancement of ocean floor observation technology for exploration of the mantle transition layer"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050012570393904000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Electrical conductivity of old oceanic mantle in the northwestern Pacific I: 1-D profiles suggesting differences in thermal structure not predictable from a plate cooling model"},{"@value":"Electrical conductivity of old oceanic mantle in the northwestern Pacific I: 1-D profiles suggesting differences in thermal structure not predictable by a plate cooling model"}]},{"@id":"https://cir.nii.ac.jp/crid/1050022457826475776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A cost-effective three-dimensional marine controlled-source electromagnetic survey: Exploring seafloor massive sulfides"}]},{"@id":"https://cir.nii.ac.jp/crid/1050303932803179136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A marine controlled-source electromagnetic application using towed and seafloor-based receivers capable of mapping seafloor and embedded massive sulfides"}]},{"@id":"https://cir.nii.ac.jp/crid/1360001114152073600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Nonlinear conjugate gradients algorithm for 2-D magnetotelluric inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232173826560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evidence for middle Triassic to Miocene dual subduction zones beneath the Shan–Thai terrane, western Thailand from magnetotelluric data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004234589649792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Practical incorporation of local and regional topography in three-dimensional inversion of deep ocean magnetotelluric data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142552422400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Probing 1-D electrical anisotropy in the oceanic upper mantle from seafloor magnetotelluric array data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013171557421952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Exploring the shallow geothermal fluid reservoir of Fang geothermal system, Thailand via a 3-D magnetotelluric survey"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025434458597376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Electrical resistivity structure at the northern margin of the Tibetan Plateau and tectonic implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025435881772928","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"3-D minimum-structure inversion of magnetotelluric data using the finite-element method and tetrahedral grids"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025437243551488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Electrically anisotropic structure of the Rocky Mountain Trench near Valemount, British Columbia inferred from magnetotellurics: implications for geothermal exploration"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025439544305792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Radiomagnetotelluric two-dimensional forward and inverse modelling accounting for displacement currents"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285709566300672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional inversion of magnetotelluric phase tensor data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286993149712768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Internal Structure of a Seafloor Massive Sulfide Deposit by Electrical Resistivity Tomography, Okinawa Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292618919228544","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Two-level dynamic scheduling in PARDISO: Improved scalability on shared memory multiprocessing systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294645687737472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional controlled-source electromagnetic and magnetotelluric joint inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294724589558656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A pilot magnetotelluric survey for geothermal exploration in Mae Chan region, northern Thailand"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298345525014656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"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/1360306909610370432","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Forward modeling and inversion of tensor CSAMT in 3D anisotropic media"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306909610687104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional magnetotelluric signatures and rheology of subducting continental crust: Insights from Sikkim Himalaya, India"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306909610694144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"3-D magnetotelluric imaging of the Phayao Fault Zone, Northern Thailand: Evidence for saline fluid in the source region of the 2014 Chiang Rai earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306909611102080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Electrically Anisotropic Crust From Three‐Dimensional Magnetotelluric Modeling in the Western Junggar, NW China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306910018750464","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Effects of 3d Electrical Anisotropy On Magnetotelluric Responses: Synthetic Case Studies"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306910246868224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Axis anisotropic Occam’s 3D inversion of tensor CSAMT in data space"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306910247076992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"2D data-space cross-gradient joint inversion of MT, gravity and magnetic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306910247077888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional magnetotelluric axial anisotropic forward modeling and inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306910247129472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Two-dimensional direct current (DC) resistivity inversion: Data space Occam's approach"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306910247238656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lithospheric Conductors Shed Light on the Non‐Uniform Destruction of North China Craton"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306910247792256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Two‐dimensional data‐space joint inversion of magnetotelluric, gravity, magnetic and seismic data with cross‐gradient constraints"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306910247980032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The influence of anisotropic electrical resistivity on surface magnetotelluric responses and the design of two new anisotropic inversions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306911085892608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evidence for an extensive intrusive component of the Deccan Large Igneous Province in the Narmada Son Lineament region, India from three dimensional magnetotelluric studies"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306911085905792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An assessment of a shallow geothermal reservoir of Mae Chan hot spring, northern Thailand via magnetotelluric surveys"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306911085964288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three dimensional conductivity model of the Tendaho High Enthalpy Geothermal Field, NE Ethiopia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306911086385408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Electrical resistivity structure of the Great Slave Lake shear zone, northwest Canada: implications for tectonic history"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306911086616448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hybrid conjugate gradient-Occam algorithms for inversion of multifrequency and multitransmitter EM data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306912165999488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetotelluric Transfer Functions: Phase Tensor and Tipper Vector above a Simple Anisotropic Three-Dimensional Conductivity Anomaly and Implications for 3D Isotropic Inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306912340663040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Electrical mantle anisotropy and crustal conductor: a 3-D conductivity model of the Rwenzori Region in western Uganda"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306914142190336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Crustal Magmatism and Anisotropy Beneath the Arabian Shield—A Cautionary Tale"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306914239836160","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three‐Dimensional Magnetotelluric Inversion for Arbitrarily Anisotropic Earth Using Unstructured Tetrahedral Discretization"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095440854912","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A set of level 3 basic linear algebra subprograms"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588383647870720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"WSJointInv2D-MT-DCR: An efficient joint two-dimensional magnetotelluric and direct current resistivity inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588384981884544","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"3D MT Anisotropic Inversion Based on Unstructured Finite-element Method"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588386274402304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Joint Inversion of Magnetotelluric Impedance and Tipper Data in 3D Axial Anisotropic Media"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588387002334080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An efficient data space conjugate gradient Occam's method for three-dimensional magnetotelluric inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588388347652736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three‐Dimensional Inversion of Magnetotelluric Data for a Resistivity Model With Arbitrary Anisotropy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588388808143616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Electrical Anisotropy Evidence in the in Ouzzal Granulitic Unit, Western Hoggar (Southern Algeria)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588388808717184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tectonic controls on magmatic systems: Evidence from a three-dimensional anisotropic electrical resistivity model of Ceboruco Volcano"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588388808739456","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional magnetotelluric inversion considering electrical anisotropy with synthetic and real data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588388809045376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Comparative 3D inversion of magnetotelluric phase tensors and impedances reveals electrically anisotropic base of Gawler Craton, South Australia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588388809293312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Artefacts of isotropic inversion applied to magnetotelluric data from an anisotropic Earth"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588389324084352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deep structural controls on the distribution of carbonate reservoirs and overburden heterogeneity in Central Luconia province, offshore Borneo revealed by 3D anisotropic inversion of regional controlled-source electromagnetic and magnetotelluric profile data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588389968011776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Data space conjugate gradient inversion for 2-D magnetotelluric data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848659519970560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A 3-D conductivity model of the Australian continent using observatory and magnetometer array data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571463181952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Computational recipes for electromagnetic inverse problems"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869858940534912","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional resistivity structure in Toya caldera region, Southwest Hokkaido, Japan — Constraints on magmatic and geothermal activities"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869864186022784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hydrothermal Reservoir and Electrical Anisotropy Investigated by Magnetotelluric Data, Case Study of Asal Rift, Republic of Djibouti"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043520930048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magmatic hydrothermal system inferred from the resistivity structure of Kusatsu-Shirane Volcano"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043927505792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Exploration for unconformity-type uranium deposits with audiomagnetotelluric data: A case study from the McArthur River mine, Saskatchewan, Canada"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520531353344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"ModEM: A modular system for inversion of electromagnetic geophysical data"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699996347528064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Role of Electrical Anisotropy in Magnetotelluric Responses: From Modelling and Dimensionality Analysis to Inversion and Interpretation"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421259662848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An efficient data-subspace inversion method for 2-D magnetotelluric data"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894485900672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A magnetotelluric study of Mount Ruapehu volcano, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895879964672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"3D magnetic data-space inversion with sparseness constraints"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370064733696","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-Dimensional Magnetotelluric Inversion: An Introductory Guide for Developers and Users"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318501739648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An efficient inversion for two-dimensional direct current resistivity surveys based on the hybrid finite difference–finite element method"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320029982848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetotelluric inversion for anisotropic conductivities in layered media"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794172989184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Correction of seafloor magnetotelluric data for topographic effects during inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795453016192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"WSINV3DMT: Vertical magnetic field transfer function inversion and parallel implementation"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269084036224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A hybrid finite difference–finite element method to incorporate topography for 2D direct current (DC) resistivity modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270877422720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Solving unsymmetric sparse systems of linear equations with PARDISO"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489937664","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-dimensional inversion for Network-Magnetotelluric data"}]},{"@id":"https://cir.nii.ac.jp/crid/1570572701503332736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Regional conductivity structure of Cascadia : Preliminary results from 3D inversion of USArray transportable array magnetotelluric data"}]},{"@id":"https://cir.nii.ac.jp/crid/1572261551242659200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-dimensional magnetotelluric inversion : Data-space method"},{"@value":"Three-dimensional magnetotelluric: data space method"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417112312064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A 3D electrical resistivity model around the focal zone of the 2017 southern Nagano Prefecture earthquake (MJMA 5.6) : implications for relationship between seismicity and crustal heterogeneity"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266985496192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetotelluric study in the Los Lagos Region (Chile) to investigate volcano-tectonic processes in the Southern Andes"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1186/s40623-024-02113-5"},{"@type":"KAKEN","@value":"PRODUCT-25590285"},{"@type":"KAKEN","@value":"PRODUCT-25355284"},{"@type":"KAKEN","@value":"PRODUCT-25600001"}]}