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

被引:1
|
作者
Zhabin, A. V. [1 ]
Belyavtseva, E. E. [1 ]
Sirotin, V. I. [1 ]
Mahfuz, Z. H. [1 ]
机构
[1] Voronezh State Univ, Voronezh 394018, Russia
关键词
D O I
10.1134/S1028334X1805032X
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
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.
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收藏
页码:573 / 574
页数:2
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