SUPERGENE CORUNDUM IN THE QUATERNARY PERMAFROST OF YAKUTIA

dc.contributor.author	Zigert Kh.
dc.contributor.author	Nikishova L.V.
dc.contributor.author	Shirokov A.L.
dc.contributor.author	Babiy O.A.
dc.contributor.author	Istomina S.V.
dc.date.accessioned	2020-10-06T05:10:44Z
dc.date.available	2020-10-06T05:10:44Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31092069
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 2, 155-159
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17763
dc.description.abstract	Corundum is formed primarily by igneous activity, and by contact and regional metamorphism. The finding of supergene corundum in syngenetically frozen sedimentary rocks of Yakutia reflects the specific characteristics of mineral generation under permafrost conditions and indicates the possibility of low-temperature generation of corundum by cryogenesis.
dc.subject	Quaternary	en
dc.title	SUPERGENE CORUNDUM IN THE QUATERNARY PERMAFROST OF YAKUTIA
dc.type	Статья
dc.subject.age	Cenozoic::Quaternary	en
dc.subject.age	Кайнозой::Четвертичная	ru

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