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


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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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