干旱区生态环境知识资源中心(Arid): Pore Space in Carbonate Tidalites: Paleoclimatic Aspect

Arid

DOI	10.1134/S0024490219040047
	Pore Space in Carbonate Tidalites: Paleoclimatic Aspect
	Kuznetsov, V. G.; Zhuravleva, L. M.
通讯作者	Kuznetsov, V. G.
来源期刊	LITHOLOGY AND MINERAL RESOURCES
ISSN	0024-4902
EISSN	1608-3229
出版年	2019
卷号	54 期号:4 页码:320-332
英文摘要	Carbonate sediments in tidal zones are characterized by microgranular textures, insignificant content of the clayey material, and abundance of the cyanobacterial formations. The arid climate fosters the formation of dolomitic tidalites in association with evaporites containing numerous stromatolite interlayers. Dolomitic tidalites make up the lower and upper elements of the three-member transgressive-regressive cyclites, whereas tidalites deposited in a humid climate are confined to the base of two-member limestone cyclites. In both cases, the pore space is created by the abundance of bacterial formations, a very specific feature responsible for the sharp anisotropy of permeability.
类型	Article
语种	英语
国家	Russia
收录类别	SCI-E
WOS记录号	WOS:000473243600004
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/2XILL650/217510
作者单位	Gubkin Russian State Univ Oil & Gas, Leninskii Pr 65-1, Moscow 119991, Russia
推荐引用方式 GB/T 7714	Kuznetsov, V. G.,Zhuravleva, L. M.. Pore Space in Carbonate Tidalites: Paleoclimatic Aspect[J],2019,54(4):320-332.
APA	Kuznetsov, V. G.,&Zhuravleva, L. M..(2019).Pore Space in Carbonate Tidalites: Paleoclimatic Aspect.LITHOLOGY AND MINERAL RESOURCES,54(4),320-332.
MLA	Kuznetsov, V. G.,et al."Pore Space in Carbonate Tidalites: Paleoclimatic Aspect".LITHOLOGY AND MINERAL RESOURCES 54.4(2019):320-332.