RADIOMETRIC DATING ON GLAUCONITE FROM DEPOSITS OF THE GLOBIGERAPSIS SEMIINVOLUTA ZONE (UPPER EOCENE) IN THE EASTERN MEDITERRANEAN

dc.contributor.author	Vinogradov V.I.
dc.contributor.author	Golovin D.I.
dc.contributor.author	Krasheninnikov V.A.
dc.date.accessioned	2020-04-10T02:20:30Z
dc.date.available	2020-04-10T02:20:30Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30954418
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 301, 4, 96-99
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16540
dc.description.abstract	Carbonate material of the glauconite-bearing horizon underwent intensive recrystallization during early diagenesis, and that glauconite is a product of that very stage of early diagenesis, and that glauconite is a product of that very stage of early diagenetic alteration. The driving force behind such processes was the decomposition of organic matter in the sediment. The glauconitic layer chosen seems optimal as a marker dating the lower boundary of the upper Eocene. The paper describes the experimental materials and procedures, and it discusses the study results.
dc.subject	Eocene	en
dc.title	RADIOMETRIC DATING ON GLAUCONITE FROM DEPOSITS OF THE GLOBIGERAPSIS SEMIINVOLUTA ZONE (UPPER EOCENE) IN THE EASTERN MEDITERRANEAN
dc.type	Статья
dc.subject.age	Cenozoic::Paleogene::Eocene	en
dc.subject.age	Кайнозой::Палеоген::Эоцен	ru

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