Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/25264
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dc.contributor.authorBandyopadhyay, Amitava-
dc.date.accessioned2014-01-06T18:34:27Z-
dc.date.available2014-01-06T18:34:27Z-
dc.date.issued2000-03-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/25264-
dc.description19-26en_US
dc.description.abstractAnalyses of shallow seismic profiles on the outer continental shelf, between Krishna and Godavari valleys off central east cost of India, reveal prograding sedimentary sequences on the shelf as well as on the flanks of the valleys. The progradation on the outer shelf is associated with palaeovalleys. A non-depositional / erosional unconformity surface has been recognised throughout the shelf at 20-25m subsurface. This is followed by a transgressive sequence of progradational sediments deposited during rising eustatic sea level accompanied by subsidence of the sea floor.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(1) [March 2000]en_US
dc.titleShelf progradation : Interpretation from seismic facies of eastern Indiaen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.29(1) [March 2000]

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