ORIGIN OF CENOMANIAN NODULAR PHOSPHORITES IN THE DNIEPER-DONETS DEPRESSION (PALEOGEOGRAPHIC ASPECT)

dc.contributor.author	Kholodov V.N.
dc.date.accessioned	2024-12-15T02:15:13Z
dc.date.available	2024-12-15T02:15:13Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13504840
dc.identifier.citation	Lithology and Mineral Resources, 2006, 41, 5, 401-416
dc.identifier.issn	0024-4902
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46973
dc.description.abstract	Paleogeographic settings of the Dnieper-Donets Depression are discussed with consideration of its Cenomanian provenance, land-sea proportions, and paleoclimate. The role of the Jurassic-Cretaceous weathering crust that stimulated the formation of phosphate solutions and the accumulation of apatite-ilmenite placer deposits is emphasized. Based on global regularities in the phosphorite formation, it is stated that weathered areas of adjacent land, rather than the World Ocean, represented the main source of phosphorus in ancient platform basins. © Pleiades Publishing, Inc. 2006.
dc.subject	Jurassic
dc.subject	Cenomanian
dc.title	ORIGIN OF CENOMANIAN NODULAR PHOSPHORITES IN THE DNIEPER-DONETS DEPRESSION (PALEOGEOGRAPHIC ASPECT)
dc.type	Статья
dc.identifier.doi	10.1134/S0024490206050014
dc.subject.age	Mesozoic::Jurassic
dc.subject.age	Мезозой::Юрская
dc.subject.age	Mesozoic::Cretaceous::Upper::Cenomanian
dc.subject.age	Мезозой::Меловая::Верхний::Сеноманский

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