UPPER CRETACEOUS DEPOSITS IN EASTERN PIEDMONTS OF THE LESSER CAUCASUS

dc.contributor.authorGasanov T.Ab.
dc.contributor.authorMelikov O.G.
dc.contributor.authorBabaev Sh.A.
dc.contributor.authorAliev G.A.
dc.date.accessioned2021-06-24T08:05:47Z
dc.date.available2021-06-24T08:05:47Z
dc.date.issued2002
dc.description.abstractThe 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.identifierhttps://elibrary.ru/item.asp?id=27764923
dc.identifier.citationStratigraphy and Geological Correlation, 2002, 10, 3, 286-294
dc.identifier.issn0869-5938
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/29304
dc.subjectCretaceous
dc.subject.ageMesozoic::Cretaceous
dc.subject.ageМезозой::Меловаяru
dc.titleUPPER CRETACEOUS DEPOSITS IN EASTERN PIEDMONTS OF THE LESSER CAUCASUS
dc.typeСтатья

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