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dc.contributor.authorGandhi, M.S.-
dc.contributor.authorSeetharamaiah, J.-
dc.contributor.authorMurthy, P. B.-
dc.date.accessioned2014-01-09T10:11:50Z-
dc.date.available2014-01-09T10:11:50Z-
dc.date.issued2000-06-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/25412-
dc.description128-132en_US
dc.description.abstractInvestigations on six vibracores collected at active sedimentation area in the southwestern margin of the lower Krishna delta indicate that the sediments are sands (3) to mud (8) , well-to-poor sorting with or without bioturbation. The presence of parallel and cross bedding and interbedded sands in the vertical facies represents intense tidal reworking and storm events, respectively. The sedimentation process and progradation of the delta are controlled by the successive repetition and formation of spits and lagoons.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.titleSediment characteristics in the depositional environments of the Krishna delta, east coast of Indiaen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.29(2) [June 2000]

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