Stratigraphy and microfossils (radiolarians and planktonic foraminifers) ofthe Upper Cretaceous (upper Santonian–lower Campanian) Struganik limestone (Western Serbia)

Bragina, L.G.; Bragin, N.Y.; Kopayevich, L.F.; Nevenka, D.; Natasaˇ, G.S.

Информация о цитировании статьи получена из Web of Science, Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 9 октября 2019 г.

Авторы: Bragina Liubov G., Bragin Nikita Yu, Kopayevich Ludmila F., Nevenka Djeric´, Natasaˇ Gerzina Spajic´
Журнал: Palaeoworld
Том: 29
Год издания: 2019
Издательство: Elsevier BV
Местоположение издательства: Netherlands
Первая страница: 361
Последняя страница: 380
DOI: 10.1016/j.palwor.2019.05.001
Аннотация: Radiolarians and planktonic foraminifers were studied from several sections of the Upper Cretaceous lithographic limestones near Struganik Village (Western Serbia). These deposits were formed in a local basin, in a low-energy sedimentary environment surrounded by a shallow-water carbonate platform. The Struganik limestone is represented by alternating micritic limestone with calcarenite, rudite and tuffaceous rocks. The sections of the Struganik limestone have a narrow stratigraphic interval that covers the upper Santonian and probably includes the lower Campanian, with a total thickness reaching 120–150 m. The radiolarian zones Crucella robusta and Afens perapediensis were traced within the unit. The foraminiferal zone Dicarinella asymetrica was tentatively identified.
Добавил в систему: Копаевич Людмила Федоровна

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Stratigraphy and microfossils (radiolarians and planktonic foraminifers) ofthe Upper Cretaceous (upper Santonian–lower Campanian) Struganik limestone (Western Serbia)статья

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