Magnetometrics in the study of sub surface structures of Antarctica margin

dc.contributor.authorArora, B.R.
dc.contributor.authorWaghmare, S.Y.
dc.contributor.authorD'Cruz, L.A.
dc.date.accessioned2015-09-15T10:44:28Z
dc.date.accessioned2021-02-12T10:41:11Z
dc.date.available2015-09-15T10:44:28Z
dc.date.available2021-02-12T10:41:11Z
dc.date.issued1985
dc.description.abstractDuring the second Indian Antartica expedition in addition to monitoring time variation in the geomagnetic field components a preliminary ground based magnetic survey was conducted Magneto metric data obtained along six 10 -15 km long profiles, after correction for transient and day- day variability are examined in the form of magnetic profiles and anomaly contour map . Qualitative interpretation of data suggests the presence of a north- south trending rift structure on the topographic ridge between 10- 12 E. The structure appears to be northward continuation of rift valley mapped on the continental margin of the Princes Astrid coast. The rift structure appears to terminate against a sharp discontinuity.en_US
dc.identifier.accession090918
dc.identifier.citationSecond Indian Expedition to Antarctica, DOD Technical Pub.No.2, p.69-73, 1985en_US
dc.identifier.urihttp://library.iigm.res.in:4000/handle/123456789/420
dc.language.isoenen_US
dc.subjectSurvey planen_US
dc.subjectEdge anomaliesen_US
dc.subjectTalwanien_US
dc.subjectMagnetometricsen_US
dc.subjectGeomagnetic fielden_US
dc.subjectAntarticaen_US
dc.titleMagnetometrics in the study of sub surface structures of Antarctica marginen_US
dc.typeArticleen_US

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