NEW AGE DATA ON KIMBERLITES FROM THE YAKUTIAN DIAMONDIFEROUS PROVINCE

dc.contributor.author	Agashev A.M.
dc.contributor.author	Pokhilenko N.P.
dc.contributor.author	Mal'kovets V.G.
dc.contributor.author	Sobolev N.V.
dc.contributor.author	Tolstov A.V.
dc.contributor.author	Polyanichko V.V.
dc.date.accessioned	2022-08-03T05:20:59Z
dc.date.available	2022-08-03T05:20:59Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13465117
dc.identifier.citation	Doklady Earth Sciences, 2004, 399, 8, 1142-1145
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38456
dc.description.abstract	Among the approximately 30 kimberlite fields discovered within the Siberian Craton, 25 make up the Yakutian kimberlite province. The study of the relationships between kimberlites and host rocks, fauna in xenoliths of the host rocks [1], and comparison of isotopic datings with different grades of reliability during the two decades after their discovery in 1954 has made it possible to distinguish three stages of Yakutian kimberlite magmatism: Middle Paleozoic (Late Devonian-Early Carboniferous), Triassic, and Late Mesozoic [2]. The fields of the southern part of the province formed in Middle Paleozoic, mainly in the Devonian. The northern part of the province mainly consists of Mesozoic kimberlite fields.
dc.title	NEW AGE DATA ON KIMBERLITES FROM THE YAKUTIAN DIAMONDIFEROUS PROVINCE
dc.type	Статья

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