REEF FORMATION IN THE GENERAL EVOLUTION OF CARBONATE ACCUMULATION

dc.contributor.author	Kuznetsov V.G.
dc.date.accessioned	2024-10-27T02:28:35Z
dc.date.available	2024-10-27T02:28:35Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13514462
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 3, 352-355
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46213
dc.description.abstract	In the model of purely biogenic mechanism, organisms make up skeletons of aragonite and calcite (including the high-magnesian variety), which are transferred to sediments after their death to provide the basis of carbonate rock. The biochemogenic mechanism is connected with the activity of photosynthesizing organisms, which consume the water-dissolved carbon dioxide, increase pH of the medium, and disturb the carbonate equilibrium, leading to the decomposition of dissolved bicarbonates and precipitation of insoluble carbonates.
dc.title	REEF FORMATION IN THE GENERAL EVOLUTION OF CARBONATE ACCUMULATION
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06030020

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