SMALL-SCALE STRATIGRAPHY IN A LARGE RAMP DELTA: RECENT AND HOLOCENE SEDIMENTATION IN THE VOLGA DELTA, CASPIAN SEA

dc.contributor.author	Overeem I.
dc.contributor.author	Kroonenberg S.B.
dc.contributor.author	Veldkamp A.
dc.contributor.author	Groenesteijn K.
dc.contributor.author	Rusakov G.V.
dc.contributor.author	Svitoch A.A.
dc.date.accessioned	2022-02-16T12:21:57Z
dc.date.available	2022-02-16T12:21:57Z
dc.date.issued	2003
dc.description.abstract	The Volga delta differs from all other major deltas in the world by its extremely gentle onshore and offshore gradient (∼5 cm/km) and by being affected by the rapid sea-level changes of the Caspian Sea, at rates up to a hundred times the global sea-level rise. This paper reports (1) the morphological and facies development of part of the lower delta during the last full sea-level cycle between 1929 and 1995, as monitored using remote sensing and field mapping, and (2) the Holocene development of the delta from outcrop data and augered transects.
dc.identifier	https://elibrary.ru/item.asp?id=13436945
dc.identifier.citation	Sedimentary Geology, 2003, 159, 3-4, 133-157
dc.identifier.issn	0037-0738
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/35453
dc.subject	Volga delta
dc.subject	Fieldwork
dc.subject	Lower delta plain
dc.subject	Sequence stratigraphy
dc.subject.age	Cenozoic::Quaternary::Holocene
dc.subject.age	Кайнозой::Четвертичная::Голоцен	ru
dc.title	SMALL-SCALE STRATIGRAPHY IN A LARGE RAMP DELTA: RECENT AND HOLOCENE SEDIMENTATION IN THE VOLGA DELTA, CASPIAN SEA
dc.type	Статья

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