TITANIUM-ZIRCONIUM PLACERS OF THE STAVROPOL REGION

dc.contributor.author	Boiko N.I.
dc.date.accessioned	2022-09-28T05:54:11Z
dc.date.available	2022-09-28T05:54:11Z
dc.date.issued	2004
dc.identifier	https://elibrary.ru/item.asp?id=13458391
dc.identifier.citation	Lithology and Mineral Resources, 2004, 39, 6, 523-529
dc.identifier.issn	0024-4902
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38783
dc.description.abstract	Lithofacies analyses and paleogeographic reconstructions of the middle Sarmatian sequence in the central Ciscaucasus, which hosts the most promising titanium–zirconium placers of the Stavropol region, indicate that ore components (rutile, ilmenite, leucoxene, and zircon) were mainly delivered to the Stavropol placer basin by the paleo-Volga River from a northern land. Bryozoan organogenic edifices played a significant role in the formation of placers. The organogenic edifices appeared under anomalous (for bioherm formation) conditions of terrigenous sedimentation on the western and northwestern slopes of the Stavropol Uplift, hampered the transport of ore material to the deep-water zone of the basin, and promoted its differentiation in the paleouplift.
dc.title	TITANIUM-ZIRCONIUM PLACERS OF THE STAVROPOL REGION
dc.type	Статья

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