New Ideas on the Origin of Chalk in Upper Cretaceous Rocks of the Voronezh Anteclise


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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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