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dc.contributor.authorGaur, A.S.
dc.contributor.authorVora, K.H.
dc.date.accessioned2009-01-10T11:19:43Z
dc.date.available2009-01-10T11:19:43Z
dc.date.issued1999
dc.identifier.citationCurrent Science, Vol.77; 180-185p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/1793
dc.description.abstractChanges in the shoreline at any point could be due to various reasons such as tectonic disturbance or shift in sedimentological regime causing erosion or deposition. Many scientific investigations, focussing on the palaeoshorelines vis-a-vis sea level fluctuations in India based on numerous geological techniques, have indicated that at about 6000 BP, the sea level was approximately 6 m higher than at present and about 4000 years BP it stabilized at the present one with minor fluctuations.
dc.language.isoen
dc.publisherCurrent Science Association, Bangalore, India
dc.rightsCopyright [1999]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
dc.subjectpalaeoshorelines
dc.subjectpalaeotopography
dc.subjectsea level changes
dc.subjecttectonics
dc.subjectsedimentology
dc.subjecterosion
dc.subjectarchaeology
dc.subjectunderwater exploration
dc.titleAncient shorelines of Gujarat, India, during the Indus civilization (Late Mid-Holocene): A study based on archaeological evidences
dc.typeJournal Article


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