CONDITIONS OF FORMATION OF CARBONATE SEQUENCES IN THE UPPER RIPHAEAN OF THE SOUTHERN URALS

dc.contributor.author	Krylov I.N.
dc.contributor.author	Zavarzin G.A.
dc.date.accessioned	2020-04-10T02:20:29Z
dc.date.available	2020-04-10T02:20:29Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30956117
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 300, 3, 207-208
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16532
dc.description.abstract	Detailed study of the upper Riphaean Min'yara formation of the southern Urals and the fossilized organic matter occurring in it enabled the author to show that the properties of these fossils correlate with several characteristics of present-day cyanobacteria communities. The Min'yara formation is as much as 800 m thick and consists of stratified dolomite and dolomitized limestone, with biostromes and bioherms of platy and columnar stromatolites. It is generally thought that rocks of this type were deposited in shallow seas in the tidal or littoral zone or somewhat below the littoral. Some of them may have been deposited in lagoons. The deposition of Min'yara formation must have occurred under similar conditions. Study methods and results are discussed.
dc.title	CONDITIONS OF FORMATION OF CARBONATE SEQUENCES IN THE UPPER RIPHAEAN OF THE SOUTHERN URALS
dc.type	Статья

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