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dc.contributor.authorWaghmare, S.Y.
dc.contributor.authorPimprikar, S.D.
dc.contributor.authorGawali, P.B.
dc.contributor.authorCarlo, L.
dc.contributor.authorPatil, A.G.
dc.date.accessioned2015-09-16T05:13:31Z
dc.date.accessioned2021-02-12T09:24:48Z-
dc.date.available2015-09-16T05:13:31Z
dc.date.available2021-02-12T09:24:48Z-
dc.date.issued2009
dc.identifier.citationJournal of Earth System Science, v.118/3, p. 261-272, 2009, doi: 10.1007/s12040-009-0011-zen_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/424-
dc.description.abstractRepeated measurements of the total geomagnetic field on the five profiles have revealed a picture of stress-induced tectonomagnetic effect in the form of secular variation of the total geomagnetic field in the tectonically and seismically active area of Jabalpur and adjoining areas of the Narmada-Son lineament (NSL), central India. For this experiment, a reference base station was established within the study area at Jabalpur. Using proton precession magnetometers with a sensitivity of 0.1 nT, simultaneous measurements of total geomagnetic field were made annually at the base and all field stations. Five cycles of repeated observations have been performed between 2003 and 2007. For data analysis, a difference method has been applied and the residuals have been calculated as secular variations of the total geomagnetic field with values ranging from ±0.1nT to about ±14.6nT/yr over the different stations. The anomalies in secular variation of the total geomagnetic field may be related to anomalous accumulation of tectonic stresses and tensions on the deep fault zones and crustal blocks due to recent geodynamic processes and active geological inhomogeneities in the NSL.en_US
dc.language.isoenen_US
dc.subjectTectonomagnetismen_US
dc.subjectGeomagnetic secular variationen_US
dc.subjectGeomagnetic repeat surveyen_US
dc.subjectPiezomagneticen_US
dc.subjectElectrokineticen_US
dc.subjectStressen_US
dc.titleTectonomagnetic study in the seismoactive area of Narmada-Son lineament, central India: Preliminary results on repeat field observationsen_US
dc.typeArticleen_US
dc.identifier.accession090922
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