ELEMENTARY STRATIGRAPHIC UNITS

dc.contributor.author	Afanasev S.L.
dc.date.accessioned	2020-12-23T08:31:35Z
dc.date.available	2020-12-23T08:31:35Z
dc.date.issued	1997
dc.identifier	https://elibrary.ru/item.asp?id=13265026
dc.identifier.citation	Stratigraphy and Geological Correlation, 1997, , 5, 501-508
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/21180
dc.description.abstract	It has been established that every tenth bed of the Upper Cretaceous-Danian flysch deposits can be traced along the southern slope of the Greater Caucasus over a distance of 1035 km. This allowed 196 synchronous markers to be established in this region. Their synchronism is based on a relative number of cyclites and confirmed by paleontologic data. The formation time of one global stratigraphic unit is assumed to average 22 ± 9 k.y.
dc.subject	Danian	en
dc.subject	Cretaceous	en
dc.title	ELEMENTARY STRATIGRAPHIC UNITS
dc.type	Статья
dc.subject.age	Cenozoic::Paleogene::Paleocene::Danian	en
dc.subject.age	Кайнозой::Палеоген::Палеоцен::Датский	ru
dc.subject.age	Mesozoic::Cretaceous	en
dc.subject.age	Мезозой::Меловая	ru

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