An Event-Based Depositional Model for the Paleocene–Eocene Sandy–Clayey–Siliceous Sequence of the Russian Platform
- Авторлар: Zorina S.O.1, Afanasieva N.I.2, Khairtdinova L.R.1
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Мекемелер:
- Institute of Geology and Petroleum Technologies of Kazan (Volga region) Federal University
- The Central Research Institute of Geology of Industrial Minerals
- Шығарылым: Том 480, № 1 (2018)
- Беттер: 547-550
- Бөлім: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/192985
- DOI: https://doi.org/10.1134/S1028334X1805001X
- ID: 192985
Дәйексөз келтіру
Аннотация
An event-based depositional model for the Paleocene—Eocene sandy–clayey–siliceous deposits of the Russian Platform was proposed. The model was based on pulsational input of pyroclastic material and intrusion of sandy injectites. These processes should be taken into account to identify the stratigraphic position of the Paleocene–Eocene lithostratigraphic units in the eastern, southeastern, and southern parts of the Russian Platform.
Авторлар туралы
S. Zorina
Institute of Geology and Petroleum Technologies of Kazan (Volga region) Federal University
Хат алмасуға жауапты Автор.
Email: svzorina@yandex.ru
Ресей, Kazan, 420008
N. Afanasieva
The Central Research Institute of Geology of Industrial Minerals
Email: svzorina@yandex.ru
Ресей, Kazan, 420097
L. Khairtdinova
Institute of Geology and Petroleum Technologies of Kazan (Volga region) Federal University
Email: svzorina@yandex.ru
Ресей, Kazan, 420008
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