ЛАГУННО-ТРАНСГРЕССИВНЫЕ ТЕРРАСЫ

dc.contributor.author	Бадюкова Е.Н.
dc.contributor.author	Соловьева Г.Д.
dc.date.accessioned	2021-12-08T07:10:29Z
dc.date.available	2021-12-08T07:10:29Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=17355774
dc.identifier.citation	Геоморфология, 2003, , 3, 36-43
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/33070
dc.description.abstract	During the sea-level rise lagoon formation is taking place if the dip of the coastal land is less than the dip of the offshore. Under such condition lagoon and coastal bar appear simultaneously. They are genetically associated and form joint transgressive system. The sediments of bar and lagoon are of different types, though their accumulation occurs at the same hypsometric level. Thence, lagoon sediments in the transgressive train have a seat rock from previous regressive phase; they are overlay by shelly and sandy loose beach deposits of the same transgressive stage as lagoon loam and have the same age. Such paragenesis should be taken into account while interpreting geological data and paleogeographical reconstructing.
dc.title	ЛАГУННО-ТРАНСГРЕССИВНЫЕ ТЕРРАСЫ
dc.type	Статья
dc.subject.udc	551.435.342

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