Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1564
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dc.contributor.authorallSvetov, B. S.; nstitute of Physics of the Earth, Russian Academy of Sciences, Troitsk, Moscow Region, Russiaen
dc.contributor.authorallKarinskij, S. D.; nstitute of Physics of the Earth, Russian Academy of Sciences, Troitsk, Moscow Region, Russiaen
dc.contributor.authorallKuksa, Y. I.; nstitute of Physics of the Earth, Russian Academy of Sciences, Troitsk, Moscow Region, Russiaen
dc.contributor.authorallOdintsov, V. I.; Institute of Terrestrial Magnetism, Jonosphere and Radio Wave Propagation, Russian Academy of Sciences, Troitsk, Moscow Region, Russiaen
dc.date.accessioned2006-09-11T07:54:16Zen
dc.date.available2006-09-11T07:54:16Zen
dc.date.issued1997-03en
dc.identifier.urihttp://hdl.handle.net/2122/1564en
dc.description.abstractElectromagnetic (EM) monitoring of geodynamic processes can be based on the two different seismo-electrical phenomena: a change in resistivity of some geological cross-sections and a generation of EM fields of internal (geodynamic) origin. Continuous observation of the natural magnetotelluric (MT) field simultaneously provides information on both such phenomena. The transfer functions between components of the MT field reflect geoelectrical section and the residual field includes the EM field of internal origin. Their variations in time give independent information on geodynamic processes. The transfer functions and the residual field can be determined by known deterministic methods, although it appears more convenient to apply the methods of adaptive data processing. They elicit information on both phenomena in real time. Continuous MT observations were carried out at the Bishkek geodynamic testing ground (Kirgizia) during 1993. Their results show how informative MT monitoring is.en
dc.format.extent2801588 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofseries2/40 (1997)en
dc.subjectelectromagnetic monitoringen
dc.subjectseismoelectrical phenomenaen
dc.subjectmagnetotelluric fielden
dc.subjecttransfer functionsen
dc.subjectadaptive data processingen
dc.titleMagnetotelluric monitoring of geodynamic processesen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamicsen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorSvetov, B. S.en
dc.contributor.authorKarinskij, S. D.en
dc.contributor.authorKuksa, Y. I.en
dc.contributor.authorOdintsov, V. I.en
dc.contributor.departmentnstitute of Physics of the Earth, Russian Academy of Sciences, Troitsk, Moscow Region, Russiaen
dc.contributor.departmentnstitute of Physics of the Earth, Russian Academy of Sciences, Troitsk, Moscow Region, Russiaen
dc.contributor.departmentnstitute of Physics of the Earth, Russian Academy of Sciences, Troitsk, Moscow Region, Russiaen
dc.contributor.departmentInstitute of Terrestrial Magnetism, Jonosphere and Radio Wave Propagation, Russian Academy of Sciences, Troitsk, Moscow Region, Russiaen
item.cerifentitytypePublications-
item.grantfulltextopen-
item.openairetypearticle-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
item.languageiso639-1en-
crisitem.classification.parent04. Solid Earth-
crisitem.author.deptGeoelectromagnetic Research Institute, Institute of Physics of the Earth, RAS, Moscow, Russia-
crisitem.author.deptnstitute of Physics of the Earth, Russian Academy of Sciences, Troitsk, Moscow Region, Russia-
crisitem.author.deptnstitute of Physics of the Earth, Russian Academy of Sciences, Troitsk, Moscow Region, Russia-
crisitem.author.deptInstitute of Terrestrial Magnetism, Jonosphere and Radio Wave Propagation, Russian Academy of Sciences, Troitsk, Moscow Region, Russia-
Appears in Collections:Annals of Geophysics
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