LITHOFACIES FEATURES AND FORMATIONAL CONDITIONS OF PALEOGENE ZEOLITE-BEARING COMPLEXES IN THE SOUTHERN RUSSIAN PLATFORM

Kholodnaya I.A.; Khardikov A.E.

dc.contributor.author	Kholodnaya I.A.
dc.contributor.author	Khardikov A.E.
dc.date.accessioned	2024-12-22T03:47:52Z
dc.date.available	2024-12-22T03:47:52Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13519173
dc.identifier.citation	Lithology and Mineral Resources, 2006, 41, 4, 324-331
dc.identifier.issn	0024-4902
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/47054
dc.description.abstract	Zeolites are represented by clinoptilolite (from 15-20 to 30-32%) in Paleogene rocks of the southern Russian Platform. Zeolite-bearing complexes formed under coastal-marine conditions of the platform type. Clinoptilolite, originated at the diagenetic stage from mud solutions predominantly at the expense of biogenic silica, belongs to the sedimentary genetic type. © Pleiades Publishing, Inc. 2006.
dc.subject	Paleogene
dc.title	LITHOFACIES FEATURES AND FORMATIONAL CONDITIONS OF PALEOGENE ZEOLITE-BEARING COMPLEXES IN THE SOUTHERN RUSSIAN PLATFORM
dc.type	Статья
dc.identifier.doi	10.1134/S0024490206040031
dc.subject.age	Cenozoic::Paleogene
dc.subject.age	Кайнозой::Палеоген