Show simple item record

dc.contributor.authorTalwani, M.
dc.contributor.authorKrishna, K.S.
dc.contributor.authorIsmaiel, M.
dc.contributor.authorDesa, M.
dc.date.accessioned18/2/2019
dc.date.accessioned2019-02-18T20:16:35Z
dc.date.available1/12/2017
dc.date.available2019-02-18T20:16:35Z
dc.date.issued2017
dc.identifier.citationMarine and Petroleum Geology, vol.88; 2017; 1123-1125
dc.identifier.issn0264-8172
dc.identifier.urihttps://doi.org/10.1016/j.marpetgeo.2016.12.009
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/7927
dc.description.abstractThis comment applauds the survey carried out by Sibuet et al. (2016) but authors believe that their principal conclusion is in error. The Northern Bay of Bengal crust is the typical oceanic crust associated with volcanic passive margins. It is not continental crust. Authors believe that the crust underlying the Eastern Bay of Bengal and Bangladesh was generated at the Rajmahal-Sylhet line after the spreading axis jumped there from the Enderby Basin in Early Cretaceous
dc.languageen
dc.publisherElsevier
dc.relation.isreferencedbySCI
dc.titleComment on a paper by Sibuet et al. (2016) entitled �Thinned continental crust intruded by volcanics beneath the northern Bay of Bengal�
dc.typeJournal Article
dc.affiliation.authorRice University, Houston, Texas 77251-1892, USA


Files in this item

FilesSizeFormatView

There are no files associated with this item.

This item appears in the following Collection(s)

Show simple item record