GLAUCONITE AT DIFFERENT STAGES OF LITHOGENESIS IN LOWER CAMBRIAN ROCKS OF WESTERN LITHUANIA

dc.contributor.author	Ivanovskaya T.A.
dc.contributor.author	Geptner A.R.
dc.date.accessioned	2022-09-28T05:54:12Z
dc.date.available	2022-09-28T05:54:12Z
dc.date.issued	2004
dc.identifier	https://elibrary.ru/item.asp?id=13452460
dc.identifier.citation	Lithology and Mineral Resources, 2004, 39, 3, 191-202
dc.identifier.issn	0024-4902
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38794
dc.description.abstract	It is shown that glauconite was mainly formed under diagenetic conditions in terrigenous–clayey rocks (Rausven Unit) of the Lower Cambrian Virbalis Formation in western Lithuania. This was preceded by bioturbation at some levels of geological column and local short-term reworking at other levels. Different forms of glauconite and its interrelation with ambient minerals in diagenesis and epigenesis are considered. A two-phase micaceous (glauconite–illite) composition of globules has been revealed and crystallochemical characteristics of each phase is presented.
dc.subject	Cambrian
dc.title	GLAUCONITE AT DIFFERENT STAGES OF LITHOGENESIS IN LOWER CAMBRIAN ROCKS OF WESTERN LITHUANIA
dc.type	Статья
dc.subject.age	Paleozoic::Cambrian
dc.subject.age	Палеозой::Кембрийская	ru

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