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New data on the magnetostratigraphy of the Jurassic–Cretaceousboundary interval, Nordvik Peninsula (northern East Siberia)статья
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: 11 декабря 2016 г.
- Авторы: Bragin V.Yu, Dzyuba O.S., Kazansky A.Yu, Shurygin B.N.
- Журнал: Russian Geology and Geophysics
- Том: 54
- Номер: 3
- Год издания: 2013
- Издательство: ELSEVIER SCIENCE BV
- Местоположение издательства: PO BOX 211, AMSTERDAM, NETHERLANDS, 1000 AE
- Первая страница: 335
- Последняя страница: 348
- DOI: 10.1016/j.rgg.2013.02.008
- Аннотация: The results of this study were used to identify a reversed polarity magnetozone, referred to as M17r, in Berriasian sections of the Nordvik Peninsula (northern East Siberia) within the normal polarity magnetozone (M18n) from previous studies. The new magnetozone embraces the Volgian–Ryazanian boundary (Chetaites chetae/C. sibiricus zonal boundary). It was also found that the former magnetozone M17r at Nordvik, which includes the C. sibiricus/Hectoroceras kochi zonal boundary should correspond to magnetozone M16r. Using magnetostratigraphic and biostratigraphic criteria proves that the Boreal C. sibiricus Zone is correlated with at least the major part of the Tethyan Tirnovella occitanica Zone, and the Boreal H. kochi Zone is correlated with the lower part of the Malbosiceras paramimounum Subzone of the Tethyan Fauriella boissieri Zone
- Добавил в систему: Казанский Алексей Юрьевич