PHYLLOSILICATES (GLAUCONITE, ILLITE, AND CHLORITE) IN TERRIGENOUS SEDIMENTS OF THE ARYMAS FORMATION (OLENEK HIGH)

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dc.contributor.author Ivanovskaya T.A.
dc.contributor.author Gor'kova N.V.
dc.contributor.author Karpova G.V.
dc.contributor.author Pokrovskaya E.V.
dc.date.accessioned 2024-12-15T02:15:26Z
dc.date.available 2024-12-15T02:15:26Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=13512697
dc.identifier.citation Lithology and Mineral Resources, 2006, 41, 6, 547-569
dc.identifier.issn 0024-4902
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/47020
dc.description.abstract It is shown that globular phyllosilicates subjected to deep categenesis are abundant in Middle Riphean sandstones and siltstones (lower subformation of the Arymas Formation) of the Olenek High. Their detailed structural-crystallochemical characteristics are given. Secondary alterations of globules and the associated pelletal minerals at different stages of lithogenesis (illitization, chloritization, ferrugination, disintegration, and so on) are considered. Structural-crystallochemical characteristics of Fe-illite and Fe2+-Mg-chlorite in globules, pellets, separate clayey strata among glauconite-bearing sandstones and siltstones (hereafter, sandy-silty rocks), and mudstone interlayers are also presented. Possible mechanisms of the formation of these minerals are discussed. © Pleiades Publishing, Inc. 2006.
dc.subject Riphean
dc.title PHYLLOSILICATES (GLAUCONITE, ILLITE, AND CHLORITE) IN TERRIGENOUS SEDIMENTS OF THE ARYMAS FORMATION (OLENEK HIGH)
dc.type Статья
dc.identifier.doi 10.1134/S0024490206060046
dc.subject.age Precambrian::Proterozoic::Riphean
dc.subject.age Докембрий::Протерозой::Рифей


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