Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/25338
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dc.contributor.authorMalleswara Rao, M.M.-
dc.contributor.authorRao, S. Jagannadha-
dc.contributor.authorVenkateswarlu, K.-
dc.contributor.authorMurthy, K.S.R.-
dc.contributor.authorMurthy, I.V. Radhakrishna-
dc.contributor.authorSubrahmanyam, A.S-
dc.date.accessioned2014-01-07T12:16:49Z-
dc.date.available2014-01-07T12:16:49Z-
dc.date.issued2000-06-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/25338-
dc.description176-178en_US
dc.description.abstractInversion of magnetic data was carried out on 40 profiles collected across the continental margin of Visakhapatnam at a spacing of about 10 km and magnetic basement map for this region is prepared. The map reveals complex anomalies particularly beneath the inner shelf with amplitudes reaching as high as 1800nT. These anomalies appear to be associated with the complex basement structure reported earlier. The significant features inferred include, (a) a shallow and highly faulted basement, in the inner shelf; (b) a NE-SW ridge-trough configuration in the mid shelf; (c) NW-SE trending basement upward off Bhimunipatnam to Kalingapatnam and (d) N-S trending shallow basement trend off Chilka lake.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.29(2) [June 2000]en_US
dc.titleBasement configuration of Visakhapatnam – Paradip continental margin from inversion of magnetic anomaliesen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.29(2) [June 2000]

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