DURATION OF THE LATERAL PARAGENETIC REEF-EVAPORITE SYSTEM FORMATION

dc.contributor.author	Baikov A.A.
dc.date.accessioned	2022-09-28T05:54:10Z
dc.date.available	2022-09-28T05:54:10Z
dc.date.issued	2004
dc.identifier	https://elibrary.ru/item.asp?id=13456795
dc.identifier.citation	Lithology and Mineral Resources, 2004, 39, 2, 135-144
dc.identifier.issn	0024-4902
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38774
dc.description.abstract	Duration of the functioning of elements of the lateral paragenetic reef–evaporite systems in Cambrian and Late Jurassic has been calculated. Discrepancy between total durations of the vertical growth of barrier reefs and evaporite formation varies by a factor of 3–50. Neither barrier reefs were growing up nor salt was deposited in halogenic basins for enormous time spans. Specific features of the reef–evaporite system should be taken into account in the estimation of ore potential (in particular, presence of sulfides of Pb, Zn, and other metals) in barrier-reef massifs.
dc.title	DURATION OF THE LATERAL PARAGENETIC REEF-EVAPORITE SYSTEM FORMATION
dc.type	Статья

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