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Please use this identifier to cite or link to this item: http://library.iigm.res.in:8080/xmlui/handle/123456789/953
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dc.contributor.authorJoseph, E. John
dc.contributor.authorIyengar, R.V.
dc.contributor.authorD'Cruz, L.A.
dc.contributor.authorSingh, B.P.
dc.date.accessioned2017-03-06T09:15:24Z
dc.date.accessioned2021-02-12T10:41:33Z-
dc.date.available2017-03-06T09:15:24Z
dc.date.available2021-02-12T10:41:33Z-
dc.date.issued1995
dc.identifier.citationJournal of geomagnetism and geoelectricity, v.47/4, p.421-430, 1995, doi: 10.5636/jgg.47.421en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/953-
dc.description.abstractSeafloor geomagnetic field variations in three components were recorded in the Bay of Bengal near the 85°E ridge, to investigate whether the negative gravity anomaly over the ridge is due to thick sedimentary deposit or due to a thick crust. Comparison of the X-, Y-and Z-variations in the vicinity of the 85°E ridge and near the continental margin suggests that a resistive thick crust underlies the 85°E ridge. The validity of conclusions arrived at from a simple inspection of magnetograms is supported by numerical calculations using a thin sheet approximation.en_US
dc.language.isoenen_US
dc.subjectGeomagnetic soundingen_US
dc.subjectBay of Bengalen_US
dc.subjectSedimentaryen_US
dc.subjectGeomagnetic fielden_US
dc.titleSeafloor geomagnetic sounding near the 85°E ridge in the bay of Bengalen_US
dc.typeArticleen_US
dc.identifier.accession091277
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