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dc.contributor.authorMartyshko, P.en
dc.contributor.authorByzov, D.en
dc.contributor.authorMartyshko, M.en
dc.date.accessioned2019-07-22T06:46:01Z-
dc.date.available2019-07-22T06:46:01Z-
dc.date.issued2017-
dc.identifier.citationMartyshko P. Algorithm for solution 3D direct and inverse problem of magnetic prospecting / P. Martyshko, D. Byzov, M. Martyshko // International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM. — 2017. — Vol. 17. — Iss. 14. — P. 11-18.en
dc.identifier.issn1314-2704-
dc.identifier.otherhttps://doi.org/10.5593/sgem2017/14/s05.002pdf
dc.identifier.other1good_DOI
dc.identifier.other4f44593b-e4c2-46d8-bd30-0bcf2a2279eepure_uuid
dc.identifier.otherhttp://www.scopus.com/inward/record.url?partnerID=8YFLogxK&scp=85032509321m
dc.identifier.urihttp://elar.urfu.ru/handle/10995/75309-
dc.description.abstractThis paper presents the integral equations of the direct problem of magnetic prospecting with respect to demagnetization. These equations are derived for a two-layer medium model. The method of determining the intensity of a secondary magnetic field for the case of magnetizing by a static field, which potential is a harmonic function, is described. The respective integral equations are written based on the theory of a simple layer potential. An iteration algorithm for solving the three-dimensional structural inverse problem of magnetic prospecting with respect to demagnetization for the sampled medium model is proposed based on the modified method of local corrections. For the method of local corrections, it is important to suggest that a change in the model field is mostly influenced by a change in the geometry of part of the object’s boundary that is the nearest to the point of observation. The main feature of this algorithm allows us to get effective technique for solution of magnetic inverse problem for medium with any numbers of layers. © SGEM 2017. All Rights Reserved.en
dc.language.isoenen
dc.publisherInternational Multidisciplinary Scientific Geoconferenceen
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.sourceInternational Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEMen
dc.subjectDEMAGNETIZATIONen
dc.subjectMAGNETIC INVERSE PROBLEMen
dc.subjectTWO-LAYER MEDIUM MODELen
dc.subjectDEMAGNETIZATIONen
dc.subjectHARMONIC FUNCTIONSen
dc.subjectINTEGRAL EQUATIONSen
dc.subjectITERATIVE METHODSen
dc.subjectMAGNETIC PROSPECTINGen
dc.subjectMAGNETISMen
dc.subjectTHREE DIMENSIONAL COMPUTER GRAPHICSen
dc.subjectDIRECT AND INVERSE PROBLEMSen
dc.subjectDIRECT PROBLEMSen
dc.subjectITERATION ALGORITHMSen
dc.subjectLAYER POTENTIALSen
dc.subjectLOCAL CORRECTIONSen
dc.subjectMAGNETIC INVERSE PROBLEMen
dc.subjectSTATIC FIELDSen
dc.subjectTWO-LAYERen
dc.subjectINVERSE PROBLEMSen
dc.titleAlgorithm for solution 3D direct and inverse problem of magnetic prospectingen
dc.typeConference Paperen
dc.typeinfo:eu-repo/semantics/conferenceObjecten
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.conference.name17th International Multidisciplinary Scientific Geoconference, SGEM 2017en
dc.conference.date29 June 2017 through 5 July 2017-
dc.identifier.doi10.5593/sgem2017/14/S05.002-
dc.identifier.scopus85032509321-
local.affiliationBulashevich Institute of Geophysics, Ekaterinburg, Russian Federationen
local.affiliationYeltsin Ural Federal University, Ekaterinburg, Russian Federationen
local.contributor.employeeМартышко Петр Сергеевичru
local.description.firstpage11-
local.description.lastpage18-
local.issue14-
local.volume17-
local.identifier.pure6015692-
local.identifier.eid2-s2.0-85032509321-
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