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

来源：

DOKLADY EARTH SCIENCES | 2018年 / 480卷 / 01期

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.

引用

页码：573 / 574

页数：2

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