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

Sethna, S.F.; Sethna, B.S.; Kothare, Prajakta; Rao, D.R.K.; Saraf, P.D.; Venkateshwarlu, M.; Patil, S.K.

dc.contributor.author	Sethna, S.F.
dc.contributor.author	Sethna, B.S.
dc.contributor.author	Kothare, Prajakta
dc.contributor.author	Rao, D.R.K.
dc.contributor.author	Saraf, P.D.
dc.contributor.author	Venkateshwarlu, M.
dc.contributor.author	Patil, S.K.
dc.date.accessioned	2015-08-24T05:48:42Z
dc.date.accessioned	2021-02-12T09:23:14Z
dc.date.available	2015-08-24T05:48:42Z
dc.date.available	2021-02-12T09:23:14Z
dc.date.issued	2001
dc.identifier.citation	Current Science, v.80/8, p.1067-1069, 2001.	en_US
dc.identifier.uri	http://localhost:8080/xmlui/handle/123456789/257
dc.description.abstract	A 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.language.iso	en	en_US
dc.subject	Palaeomagnetic evidence	en_US
dc.subject	Tectonic deformation	en_US
dc.subject	Deccan volcanic province	en_US
dc.subject	Tectonic drag deformation	en_US
dc.subject	Western India	en_US
dc.title	A note on palaeomagnetic evidence to show tectonic deformation in the Deccan Volcanic Province of Saurashtra, western India	en_US
dc.type	Article	en_US
dc.identifier.accession	090744