ОСОБЕННОСТИ РАЗВИТИЯ ЧЕРНОМОРСКОГО ПОБЕРЕЖЬЯ ТАМАНСКОГО ПОЛУОСТРОВА В ПОЗДНЕМ ГОЛОЦЕНЕ

dc.contributor.author	Поротов А.В.
dc.contributor.author	Горлов Ю.В.
dc.contributor.author	Янина Т.А.
dc.contributor.author	Фуаш Э.
dc.date.accessioned	2022-05-08T02:20:22Z
dc.date.available	2022-05-08T02:20:22Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=17345356
dc.identifier.citation	Геоморфология, 2004, , 4, 63-77
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/37457
dc.description.abstract	The paper deals with the results of paleogeographical study of marine and deltaic sediments of the Black Sea’s shoreline of Taman’ peninsular, aimed to reconstruction of the local variation of the sea level changes and coast development in the Late Holocene. On the basis of litho-facial, palaeontological, geochronological and submarine archaeological studies an estimation of local neotectonic impact on the sea level changes for the last 5.0 ka was obtained and the time frame of recent coastal feature’s generation was determined.
dc.subject	Holocene
dc.title	ОСОБЕННОСТИ РАЗВИТИЯ ЧЕРНОМОРСКОГО ПОБЕРЕЖЬЯ ТАМАНСКОГО ПОЛУОСТРОВА В ПОЗДНЕМ ГОЛОЦЕНЕ
dc.type	Статья
dc.subject.udc	551.435.3(470.62)
dc.subject.age	Cenozoic::Quaternary::Holocene
dc.subject.age	Кайнозой::Четвертичная::Голоцен	ru

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