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dc.contributor.authorHarikumar, P.
dc.contributor.authorRajaram, M.
dc.contributor.authorBalakrishnan, T.S.
dc.date.accessioned2015-05-18T06:02:06Z
dc.date.accessioned2021-02-12T10:44:01Z-
dc.date.available2015-05-18T06:02:06Z
dc.date.available2021-02-12T10:44:01Z-
dc.date.issued2000
dc.identifier.citationJournal of Earth System Science, v.109/3, p. 381-391, 2000, doi: 10.1007/BF02702209en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/89-
dc.description.abstractThe degree sheet Aeromagnetic maps up to 17‡N, acquired from the Geological Survey of India, have been manually redigitised at 6 minute intervals to study the long wavelength anomalies over peninsular India. These data have been collected at different survey altitude, epochs, flight line directions, etc. Great care has been taken to correct the total field map and remove the contribution due to the core field and prepare an accurate crustal anomaly map. For the first time, a regional map, depicting the NW-SE structural features north of the orthopyroxene isograd with the essentially E-W features to the south of it and revealing several well known structures, is presented. The analytical signal is calculated to delineate the source fields of these anomalies. It dramatically maps the charnockites and is able to delineate the orthopyroxene isograd. In the Dharwar region the magnetic signatures are associated with the intrusives/ iron ore bodies. Thus, we find that the source rocks of the aeromagnetic anomalies are the host province of charnockites in the SGT and the intrusives/iron ore bodies in the Dharwar belt. Gravity residuals are calculated and a tectonic map of the region is presented from the combined geopotential data.en_US
dc.language.isoenen_US
dc.subjectAeromagneticen_US
dc.subjectSouthern granulite terrainen_US
dc.subjectIGRFen_US
dc.subjectAnalytical signalen_US
dc.subjectMetamorphismen_US
dc.titleAeromagnetic study of peninsular Indiaen_US
dc.typeArticleen_US
dc.identifier.accession090582
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