Email this article New Ideas on the Origin of Chalk in Upper Cretaceous Rocks of the Voronezh Anteclise
- Authors: Zhabin A.V.1, Belyavtseva E.E.1, Sirotin V.I.1, Mahfuz Z.H.1
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Affiliations:
- Voronezh State University
- Issue: Vol 480, No 1 (2018)
- Pages: 573-574
- Section: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/193028
- DOI: https://doi.org/10.1134/S1028334X1805032X
- ID: 193028
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Abstract
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.
About the authors
A. V. Zhabin
Voronezh State University
Email: belyavcevaee@yandex.ru
Russian Federation, Voronezh, 394018
E. E. Belyavtseva
Voronezh State University
Author for correspondence.
Email: belyavcevaee@yandex.ru
Russian Federation, Voronezh, 394018
V. I. Sirotin
Voronezh State University
Email: belyavcevaee@yandex.ru
Russian Federation, Voronezh, 394018
Z. H. Mahfuz
Voronezh State University
Email: belyavcevaee@yandex.ru
Russian Federation, Voronezh, 394018
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