New Ideas on the Origin of Chalk in Upper Cretaceous Rocks of the Voronezh Anteclise
- 作者: Zhabin A.V.1, Belyavtseva E.E.1, Sirotin V.I.1, Mahfuz Z.H.1
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隶属关系:
- Voronezh State University
- 期: 卷 480, 编号 1 (2018)
- 页面: 573-574
- 栏目: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/193028
- DOI: https://doi.org/10.1134/S1028334X1805032X
- ID: 193028
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详细
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.
作者简介
A. Zhabin
Voronezh State University
Email: belyavcevaee@yandex.ru
俄罗斯联邦, Voronezh, 394018
E. Belyavtseva
Voronezh State University
编辑信件的主要联系方式.
Email: belyavcevaee@yandex.ru
俄罗斯联邦, Voronezh, 394018
V. Sirotin
Voronezh State University
Email: belyavcevaee@yandex.ru
俄罗斯联邦, Voronezh, 394018
Z. Mahfuz
Voronezh State University
Email: belyavcevaee@yandex.ru
俄罗斯联邦, Voronezh, 394018
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