An algorithm for the three‐dimensional inversion of magnetotelluric data
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Résumé
PreviousNext No AccessSEG Technical Program Expanded Abstracts 2002An algorithm for the three‐dimensional inversion of magnetotelluric dataAuthors: Colin G. FarquharsonDouglas W. OldenburgEldad HaberRoman ShekhtmanColin G. FarquharsonUBC‐Geophysical Inversion Facility, U. of British Columbia, Vancouver, Canada, Douglas W. OldenburgUBC‐Geophysical Inversion Facility, U. of British Columbia, Vancouver, Canada, Eldad HaberEMI‐Schlumberger, Richmond, CA, and Roman ShekhtmanUBC‐GIFhttps://doi.org/10.1190/1.1817336 SectionsAboutPDF/ePub ToolsAdd to favoritesDownload CitationsTrack CitationsPermissions ShareFacebookTwitterLinked InReddit Permalink: https://doi.org/10.1190/1.1817336FiguresReferencesRelatedDetailsCited byHybrid mesh for magnetotelluric forward modeling based on the finite element method11 January 2023 | Scientific Reports, Vol. 13, No. 1Fast 3D simulation of magnetotelluric data in anisotropic media using a rational Krylov methodJunjun Zhou, Ningbo Bai, Xiangyun Hu, Tiaojie Xiao, and Zhidan Long17 October 2023 | GEOPHYSICS, Vol. 88, No. 6Processing of passive EM fields acquired during active-source airborne EM surveys4 February 2021 | Exploration Geophysics, Vol. 52, No. 6An efficient parallel algorithm for 3D magnetotelluric modeling with edge-based finite element6 July 2020 | Computational Geosciences, Vol. 25, No. 1A reduced order approach for probabilistic inversions of 3-D magnetotelluric data I: general formulation1 September 2020 | Geophysical Journal International, Vol. 223, No. 33D inversion of magnetotelluric data by using a hybrid forward-modeling approach and mesh decouplingDeniz Varılsüha11 September 2020 | GEOPHYSICS, Vol. 85, No. 5Subsurface Characterization of the Pennsylvanian Clare Basin, Western Ireland, by Means of Joint Interpretation of Electromagnetic Geophysical Data and Well‐Log Data9 July 2019 | Journal of Geophysical Research: Solid Earth, Vol. 124, No. 7Modeling sferic signals extracted from active-source AEM dataDaniel Sattel and Eric Battig27 August 2018Removal of galvanic distortion effects in 3D magnetotelluric data by an equivalent source techniqueWenwu Tang, Yaoguo Li, Douglas W. 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Oldenburg, and Jianxin Liu5 August 2014The inability of magnetotelluric off-diagonal impedance tensor elements to sense oblique conductors in three-dimensional inversion17 December 2013 | Geophysical Journal International, Vol. 196, No. 3Magnetotelluric 3-D inversion—a review of two successful workshops on forward and inversion code testing and comparison14 March 2013 | Geophysical Journal International, Vol. 193, No. 3Methods and algorithms for reconstructing three-dimensional distributions of electric conductivity and polarization in the medium by finite-element 3D modeling using the data of electromagnetic sounding8 May 2013 | Izvestiya, Physics of the Solid Earth, Vol. 49, No. 3The modeling of ZTEM data with 2D and 3D algorithmsDaniel Sattel and Ken Witherly25 October 2012Large-scale inversion of ZTEM dataElliot Holtham and Douglas W. Oldenburg9 July 2012 | GEOPHYSICS, Vol. 77, No. 4Electrical resistivity structure at the northern margin of the Tibetan Plateau and tectonic implications7 December 2011 | Journal of Geophysical Research, Vol. 116, No. B12Application of the 3D magnetotelluric inversion code in a geologically complex area9 June 2010 | Geophysical Prospecting, Vol. 58, No. 6Three‐dimensional inversion of MT and ZTEM dataElliot Holtham and Douglas W. Oldenburg21 October 2010Constructing piecewise-constant models in multidimensional minimum-structure inversionsColin G. Farquharson26 December 2007 | GEOPHYSICS, Vol. 73, No. 1Three‐dimensional forward modelling and inversion of Z‐TEM dataElliot Holtham and Douglas W. Oldenburg15 December 2008Constructing piecewise‐constant models in multi‐dimensional minimum‐structure inversionsColin G. Farquharson6 October 2006Three-Dimensional Electromagnetic Modelling and Inversion from Theory to ApplicationSurveys in Geophysics, Vol. 26, No. 6Three‐dimensional inversion of MT data from the Turquoise Ridge mine, NevadaColin G. Farquharson, Douglas W. Oldenburg, and Peter Kowalczyk3 January 2005 SEG Technical Program Expanded Abstracts 2002 ISSN (print):1052-3812 ISSN (online):1949-4645 Copyright: 2002 Pages: 2478 publication data© 2002 Copyright © 2002 Society of Exploration GeophysicistsPublisher:Society of Exploration Geophysicists HistoryPublished Online: 03 Jan 2005 CITATION INFORMATION Colin G. Farquharson, Douglas W. Oldenburg, Eldad Haber, and Roman Shekhtman, (2002), "An algorithm for the three‐dimensional inversion of magnetotelluric data," SEG Technical Program Expanded Abstracts : 649-652. https://doi.org/10.1190/1.1817336 Plain-Language Summary PDF DownloadLoading ...
Récupéré en direct depuis OpenAlex et désinversé. Les résumés ne sont pas conservés dans cette base de données : les index inversés représentent 8,6 Go des 9,3 Go de texte de la base, et le serveur dispose de 13 Go libres.
Comment cette classification a été obtenuedéplier
Prédiction distillée sur la base complète
Imitation des enseignantsNi prévalence calibrée, ni vérité terrain. Validation humaine à venir. Apprise à partir de 10 348 étiquettes directes de Codex et de 10 348 étiquettes directes de Gemma. Le mode candidate est l'union des têtes enseignantes seuillées; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont ni des étiquettes humaines ni des étiquettes directes de modèles de pointe.
Scores Codex et Gemma par catégorie
| Catégorie | Codex | Gemma |
|---|---|---|
| Métarecherche | 0,000 | 0,000 |
| Méta-épidémiologie (sens strict) | 0,000 | 0,000 |
| Méta-épidémiologie (sens large) | 0,000 | 0,000 |
| Bibliométrie | 0,000 | 0,000 |
| Études des sciences et des technologies | 0,000 | 0,000 |
| Communication savante | 0,000 | 0,000 |
| Science ouverte | 0,000 | 0,000 |
| Intégrité de la recherche | 0,000 | 0,000 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,005 | 0,000 |
Scores machine (provisoires)
Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.
Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.
score_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découleClassification
machine, non validéePrédiction automatique; un appel candidat d’une seule tête enseignante, pas un consensus.
Le détail, modèle par modèle et score par score, se trouve en fin de page sous « Comment cette classification a été obtenue ».