A note on palaeomagnetic evidence to show tectonic deformation in the Deccan Volcanic Province of Saurashtra, western India

dc.contributor.authorSethna, S.F.
dc.contributor.authorSethna, B.S.
dc.contributor.authorKothare, Prajakta
dc.contributor.authorRao, D.R.K.
dc.contributor.authorSaraf, P.D.
dc.contributor.authorVenkateshwarlu, M.
dc.contributor.authorPatil, S.K.
dc.date.accessioned2015-08-24T05:48:42Z
dc.date.accessioned2021-02-12T09:23:14Z
dc.date.available2015-08-24T05:48:42Z
dc.date.available2021-02-12T09:23:14Z
dc.date.issued2001
dc.description.abstractA long curved dyke with peculiar vertical layering, in the Deccan VolcanicProvince of Saurashtra, was palaeomagnetically investigated. Palaeomagnetic measurements clearly indicate that the curved character of the dyke is due to some kind of tectonic drag deformation. Such deformation could have possibly developed in case the Saurashtra Peninsula has moved northwards along the Cambay Basin fault. There is a possibility that the horst in the southern part of Saurashtra may have been originally the continuation of the Satpura horst.en_US
dc.identifier.accession090744
dc.identifier.citationCurrent Science, v.80/8, p.1067-1069, 2001.en_US
dc.identifier.urihttp://library.iigm.res.in:4000/handle/123456789/257
dc.language.isoenen_US
dc.subjectPalaeomagnetic evidenceen_US
dc.subjectTectonic deformationen_US
dc.subjectDeccan volcanic provinceen_US
dc.subjectTectonic drag deformationen_US
dc.subjectWestern Indiaen_US
dc.titleA note on palaeomagnetic evidence to show tectonic deformation in the Deccan Volcanic Province of Saurashtra, western Indiaen_US
dc.typeArticleen_US

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