PARTICIPATION OF MICROORGANISMS IN THE FORMATION OF TRAVERTINES AND SAPROPELITE KEROGEN IN SEDIMENTS OF THERMAL CARBONIC WATERS IN THE BAIKAL RIFT ZONE

dc.contributor.author	Tatarinov A.V.
dc.contributor.author	Yalovik L.I.
dc.contributor.author	Danilova E.V.
dc.contributor.author	Namsaraev Z.B.
dc.date.accessioned	2024-11-02T11:07:53Z
dc.date.available	2024-11-02T11:07:53Z
dc.date.issued	2006
dc.description.abstract	The geomicrobiological study of travertine sediments from hot springs of nitrogen sodium–sulfate waters in the Baikal rift zone demonstrated the decisive role of cyanobacterial mats in their formation. At the same time, the mechanism of decompression formation without the participation of microorganisms is assumed for travertines that are widespread in the East Sayan terrain of hot and cold carbonic waters.
dc.identifier	https://www.elibrary.ru/item.asp?id=13522755
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 9, 1435-1438
dc.identifier.doi	10.1134/S1028334X06090224
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46364
dc.title	PARTICIPATION OF MICROORGANISMS IN THE FORMATION OF TRAVERTINES AND SAPROPELITE KEROGEN IN SEDIMENTS OF THERMAL CARBONIC WATERS IN THE BAIKAL RIFT ZONE
dc.type	Статья

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