New Ideas on the Origin of Chalk in Upper Cretaceous Rocks of the Voronezh Anteclise
- Авторы: Zhabin A.V.1, Belyavtseva E.E.1, Sirotin V.I.1, Mahfuz Z.H.1
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Учреждения:
- Voronezh State University
- Выпуск: Том 480, № 1 (2018)
- Страницы: 573-574
- Раздел: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/193028
- DOI: https://doi.org/10.1134/S1028334X1805032X
- ID: 193028
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Аннотация
On the basis of the lithological and mineral composition of chalk, it is concluded that it was formed under various facial conditions. Carbonate sediment accumulated at a shallow depth and underwent wave movements. No correlation is found between the lithological chalk types and the facial conditions of precipitation of the carbonate sediment.
Об авторах
A. Zhabin
Voronezh State University
Email: belyavcevaee@yandex.ru
Россия, Voronezh, 394018
E. Belyavtseva
Voronezh State University
Автор, ответственный за переписку.
Email: belyavcevaee@yandex.ru
Россия, Voronezh, 394018
V. Sirotin
Voronezh State University
Email: belyavcevaee@yandex.ru
Россия, Voronezh, 394018
Z. Mahfuz
Voronezh State University
Email: belyavcevaee@yandex.ru
Россия, Voronezh, 394018
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