ConodontBased Stratigraphy of the Mosolovian Stage (Eifelian, Middle Devonian) of the Voronezh Anteclise

Nazarova, V.M.; Kononova, L.I.

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: 26 сентября 2016 г.

Авторы: Nazarova V.M., Kononova L.I.
Журнал: Stratigraphy and Geological Correlation
Том: 24
Номер: 4
Год издания: 2016
Издательство: Pleiades Publishing, Inc.
Местоположение издательства: New York, USA
Первая страница: 339
Последняя страница: 363
DOI: 10.1134/S0869593816030047
Аннотация: Conodonts from the deposits of the Mosolovian Regional Stage (Middle Devonian) of the Voronezh Anteclise are studied on the basis of the data from six boreholes. Three assemblages are recognized. The index species of the lowermost assemblage is Icriodus formosus Naz. The index species of the middle assemblage are I. formosus Naz. and Pseudobipennatus ziegleri Kon. et Kim, as well as I. arkonensis Stauff. and I. jejunus Naz. This assemblage is the most diverse and is recognized in all boreholes. The deposits containing this assemblage correspond to the maximum of the Nara transgression. The upper assemblage is also recognized in all the studied boreholes. Its index species is Ps. ziegleri Kon. et Kim. The Mosolovian Regional Stage is assigned to the kockelianus Zone. The distribution diagrams of species in the most diverse middle assemblage support the hypothesis that, in the southeastern regions of the Voronezh anteclise, the depth was greater than in its western part. The characteristic conodont species are shown in the plates.
Добавил в систему: Назарова Валентина Михайловна

	ИСТИНА	Войти в систему Регистрация
	ИПМех РАН
	Главная Поиск Статистика О проекте Помощь

ИСТИНА

ИПМех РАН

ConodontBased Stratigraphy of the Mosolovian Stage (Eifelian, Middle Devonian) of the Voronezh Antecliseстатья

Прикрепленные файлы