| Форма представления | Статьи в зарубежных журналах и сборниках |
| Год публикации | 2018 |
| Язык | английский |
|
Арефьев Михаил Павлович, автор
Бакаев Александр Сергеевич, автор
Буланов Валерий Викторович, автор
Иванов Александр Олегович, автор
Муравьев Федор Александрович, автор
Силантьев Владимир Владимирович, автор
|
|
Жаринова Вероника Владимировна, автор
Уразаева Миляуша Назимовна, автор
|
| Библиографическое описание на языке оригинала |
Silantiev, V., Arefiev, M., Mouraviev, F., Bulanov, V., Ivanov, A., Urazaeva, M., Bakaev, A., Zharinova, V. (2018). The Parastratotype of the Urzhumian Stage in the Vyatka-Kazan Region,
East-European Platform / In book: Barclay, M., Nikolaeva, S., Silantiev, V. (Eds.) Kazan Golovkinsky Stratigraphic Meeting, 2017: Advances in Devonian, Carboniferous and Permian Research: Stratigraphy, Environments, Climate and Resources. Filodiritto International Proceedings, Bologna, Italy, pp. 206-215.
|
| Аннотация |
New multidisciplinary studies of the Urzhumian parastratotype confirm its reference status for the
Vyatka-Kazan region of European Russia. The purely continental Urzhumian represents the upper
unit of the Biarmian Series (Middle Permian) of the Geological Time Scale of Russia and is
tentatively correlated with the Wordian of the International Chronostratigraphic Chart.
The lower part of the parastratotype corresponds to the Sulitsa Formation and consists of lacustrine
red-bed continental rocks containing rare conchostracans and fish scales. The upper part of the
parastratotype corresponds to the Isheevo Formation and is composed of red-colored alluviallacustrine
terrigenous and clayey rocks with interbeds of microbial limestones. The clayey rocks often
include a large number of paleosols of differing maturity, among which vertisols and calcisols prevail.
This part of the section contains a diverse fauna of non-marine ostracodes, bivalves,
conchostracans, fishes and tetrapods. |
| Ключевые слова |
Middle Permian, Urzhumian, biostratigraphy, non-marine bivalves, ostracodes, conchostracans, fish, tetrapods |
| Название журнала |
IOP Conference Series: Earth and Environmental Science
|
| URL |
http://www.filodirittoeditore.com/index.php?route=product/product&product_id=160 |
| Пожалуйста, используйте этот идентификатор, чтобы цитировать или ссылаться на эту карточку |
https://repository.kpfu.ru/?p_id=181983 |
Полная запись метаданных  |
| Поле DC |
Значение |
Язык |
| dc.contributor.author |
Арефьев Михаил Павлович |
ru_RU |
| dc.contributor.author |
Бакаев Александр Сергеевич |
ru_RU |
| dc.contributor.author |
Буланов Валерий Викторович |
ru_RU |
| dc.contributor.author |
Иванов Александр Олегович |
ru_RU |
| dc.contributor.author |
Муравьев Федор Александрович |
ru_RU |
| dc.contributor.author |
Силантьев Владимир Владимирович |
ru_RU |
| dc.contributor.author |
Жаринова Вероника Владимировна |
ru_RU |
| dc.contributor.author |
Уразаева Миляуша Назимовна |
ru_RU |
| dc.date.accessioned |
2018-01-01T00:00:00Z |
ru_RU |
| dc.date.available |
2018-01-01T00:00:00Z |
ru_RU |
| dc.date.issued |
2018 |
ru_RU |
| dc.identifier.citation |
Silantiev, V., Arefiev, M., Mouraviev, F., Bulanov, V., Ivanov, A., Urazaeva, M., Bakaev, A., Zharinova, V. (2018). The Parastratotype of the Urzhumian Stage in the Vyatka-Kazan Region,
East-European Platform / In book: Barclay, M., Nikolaeva, S., Silantiev, V. (Eds.) Kazan Golovkinsky Stratigraphic Meeting, 2017: Advances in Devonian, Carboniferous and Permian Research: Stratigraphy, Environments, Climate and Resources. Filodiritto International Proceedings, Bologna, Italy, pp. 206-215.
|
ru_RU |
| dc.identifier.uri |
https://repository.kpfu.ru/?p_id=181983 |
ru_RU |
| dc.description.abstract |
IOP Conference Series: Earth and Environmental Science |
ru_RU |
| dc.description.abstract |
New multidisciplinary studies of the Urzhumian parastratotype confirm its reference status for the
Vyatka-Kazan region of European Russia. The purely continental Urzhumian represents the upper
unit of the Biarmian Series (Middle Permian) of the Geological Time Scale of Russia and is
tentatively correlated with the Wordian of the International Chronostratigraphic Chart.
The lower part of the parastratotype corresponds to the Sulitsa Formation and consists of lacustrine
red-bed continental rocks containing rare conchostracans and fish scales. The upper part of the
parastratotype corresponds to the Isheevo Formation and is composed of red-colored alluviallacustrine
terrigenous and clayey rocks with interbeds of microbial limestones. The clayey rocks often
include a large number of paleosols of differing maturity, among which vertisols and calcisols prevail.
This part of the section contains a diverse fauna of non-marine ostracodes, bivalves,
conchostracans, fishes and tetrapods. |
ru_RU |
| dc.language.iso |
ru |
ru_RU |
| dc.subject |
Middle Permian |
ru_RU |
| dc.subject |
Urzhumian |
ru_RU |
| dc.subject |
biostratigraphy |
ru_RU |
| dc.subject |
non-marine bivalves |
ru_RU |
| dc.subject |
ostracodes |
ru_RU |
| dc.subject |
conchostracans |
ru_RU |
| dc.subject |
fish |
ru_RU |
| dc.subject |
tetrapods |
ru_RU |
| dc.title |
The Parastratotype of the Urzhumian Stage in the Vyatka-Kazan Region, East-European Platform |
ru_RU |
| dc.type |
Статьи в зарубежных журналах и сборниках |
ru_RU |
|
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