Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/5862
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dc.contributor.authorSingh, Raj Pal-
dc.contributor.authorKumar, Manoj-
dc.contributor.authorSingh, O P-
dc.contributor.authorSingh, Birbal-
dc.date.accessioned2009-08-10T08:29:01Z-
dc.date.available2009-08-10T08:29:01Z-
dc.date.issued2009-08-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/5862-
dc.description220-226en_US
dc.description.abstract A borehole antenna has been installed at Agra (latitude 27.2oN, longitude 78oE), India since 01 June 2006. The subsurface very low frequency (VLF) electric field emissions (f = 3.042 kHz) data has been recorded round the clock for a period of nineteen months from 01 June 2006 to 31 December 2007. This statistical analysis of data is presented in the paper. The occasional amplitude enhancement is observed in the data and examined in the light of magnetic storms, earthquakes, and lightning activities. It is found that in majority of the cases, amplitude anomalies are correlated with moderate seismic activities occurred during the period in the region. The propagation mechanism of VLF signals from the hypocenters of earthquakes to the observing station is discussed in the paper. en_US
dc.language.isoen_USen_US
dc.publisherCSIRen_US
dc.relation.ispartof91.30.paen_US
dc.sourceIJRSP Vol.38(4) [August 2009]en_US
dc.subjectEarthquakeen_US
dc.subjectVLF electric field emissionsen_US
dc.subjectBorehole antennaen_US
dc.titleSubsurface VLF electric field emissions associated with regional earthquakesen_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.38(4) [August 2009]

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