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.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.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.subject	Volga delta
dc.subject	Fieldwork
dc.subject	Lower delta plain
dc.subject	Sequence stratigraphy
dc.title	SMALL-SCALE STRATIGRAPHY IN A LARGE RAMP DELTA: RECENT AND HOLOCENE SEDIMENTATION IN THE VOLGA DELTA, CASPIAN SEA
dc.type	Статья
dc.subject.age	Cenozoic::Quaternary::Holocene
dc.subject.age	Кайнозой::Четвертичная::Голоцен	ru

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