中文版 | English
Arid
DOI10.1134/S0024490206060010
Cyclicity of shallow-water carbonate sediments in different climatic zones
Kuznetsov, V. G.
通讯作者Kuznetsov, V. G.
来源期刊LITHOLOGY AND MINERAL RESOURCES
ISSN0024-4902
EISSN1608-3229
出版年2006
卷号41期号:6页码:505-517
英文摘要

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.


类型Article
语种英语
国家Russia
收录类别SCI-E
WOS记录号WOS:000241686700001
WOS类目Geochemistry & Geophysics ; Geology ; Mineralogy
WOS研究方向Geochemistry & Geophysics ; Geology ; Mineralogy
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/152444
作者单位(1)Russian Acad Sci, Inst Oil & Gas Problems, Moscow 117701, Russia
推荐引用方式
GB/T 7714		 Kuznetsov, V. G.. Cyclicity of shallow-water carbonate sediments in different climatic zones[J],2006,41(6):505-517.
APA Kuznetsov, V. G..(2006).Cyclicity of shallow-water carbonate sediments in different climatic zones.LITHOLOGY AND MINERAL RESOURCES,41(6),505-517.
MLA Kuznetsov, V. G.."Cyclicity of shallow-water carbonate sediments in different climatic zones".LITHOLOGY AND MINERAL RESOURCES 41.6(2006):505-517.
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