CYCLICITY OF SHALLOW-WATER CARBONATE SEDIMENTS IN DIFFERENT CLIMATIC ZONES

Kuznetsov V.G.

dc.contributor.author	Kuznetsov V.G.
dc.date.accessioned	2024-12-22T03:48:02Z
dc.date.available	2024-12-22T03:48:02Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13526201
dc.identifier.citation	Lithology and Mineral Resources, 2006, 41, 6, 505-517
dc.identifier.issn	0024-4902
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/47089
dc.description.abstract	Based on the study of several different-age shallow-water carbonate sediments from different regions, it is established that cyclothems formed in basins of arid and humid climatic zones differ in their composition and structure. It is shown that the influence of climate was indirect. The climate governed salinity (particularly, in extremely shallow-water settings of initial and terminal stages of the formation of cyclothems) and, thus, stimulated changes in the biota. The biota, in turn, controlled the composition of carbonate material and mechanisms of its sedimentation. © Pleiades Publishing, Inc. 2006.
dc.title	CYCLICITY OF SHALLOW-WATER CARBONATE SEDIMENTS IN DIFFERENT CLIMATIC ZONES
dc.type	Статья
dc.identifier.doi	10.1134/S0024490206060010