UPPER CRETACEOUS DEPOSITS IN EASTERN PIEDMONTS OF THE LESSER CAUCASUS

dc.contributor.author	Gasanov T.Ab.
dc.contributor.author	Melikov O.G.
dc.contributor.author	Babaev Sh.A.
dc.contributor.author	Aliev G.A.
dc.date.accessioned	2021-06-24T08:05:47Z
dc.date.available	2021-06-24T08:05:47Z
dc.date.issued	2002
dc.identifier	https://elibrary.ru/item.asp?id=27764923
dc.identifier.citation	Stratigraphy and Geological Correlation, 2002, 10, 3, 286-294
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/29304
dc.description.abstract	The Upper Cretaceous sequence in the east of the Lesser Caucasus, within the Azerbaijan territory, begins with the Cenomanian terrigenous sediments that are overlain with a hiatus by thick volcanogenic-terrigenous deposits of the Coniacian and Santonian stages. The Campanian-Maastrichtian interval and lower Paleocene are composed mainly of limestones bearing echinoids, inocerams, and planktonic foraminifers, which are used to distinguish the substages. Boreholes between the Agdam and Fizuli cities and near the town of Terter recovered the Maastrichtian and lower Paleocene limestones below the Akchagylian cover.
dc.subject	Cretaceous
dc.title	UPPER CRETACEOUS DEPOSITS IN EASTERN PIEDMONTS OF THE LESSER CAUCASUS
dc.type	Статья
dc.subject.age	Mesozoic::Cretaceous
dc.subject.age	Мезозой::Меловая	ru

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