Please use this identifier to cite or link to this item: http://localhost:8081/jspui/handle/123456789/17155
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dc.contributor.authorYadav, Pradip Kumar-
dc.date.accessioned2025-06-25T13:13:38Z-
dc.date.available2025-06-25T13:13:38Z-
dc.date.issued2014-06-
dc.identifier.urihttp://localhost:8081/jspui/handle/123456789/17155-
dc.description.abstractMagnetometric Resistivity Method is based on measurement of low level(lOOmilligamma) and low frequency(l-5Hz) magnetic field based on direct current flow in the ground In this method we measure the magnetic field in the vicinity of one or more grounded electrodes. It has been shown that horizontally layered earth yields no MMR anomaly. The characteristic anomaly for vertical and dipping contact are represented in detail. The two factors on which MMR anomaly basically depends are-geometry and conductivity contrast. To illustrate the effect of geometry, types curves are given for very large conductivity contrast and ancillary curves gives gives conductivity contrasten_US
dc.description.sponsorshipINDIAN INSTITUTE OF TECHNOLOGY ROORKEEen_US
dc.language.isoenen_US
dc.publisherI I T ROORKEEen_US
dc.subjectMagnetometric Resistivity Methoden_US
dc.subjectGrounded Electrodesen_US
dc.subjectVerticalen_US
dc.subjectMMR Anomalyen_US
dc.titleMAGNETOMETRIC RESISTIVITY MODELLING AND ITS APPLICATIONSen_US
dc.typeOtheren_US
Appears in Collections:MASTERS' THESES (Earth Sci.)

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