TIMING AND DURATION OF KIMBERLITIC MAGMATISM IN THE ZIMNII BEREG DIAMONDIFEROUS PROVINCE: EVIDENCE FROM RB-SR AGE DATA ON KIMBERLITE SILLS ALONG THE MELA RIVER

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dc.contributor.author Pervov V.A.
dc.contributor.author Larchenko V.A.
dc.contributor.author Minchenko G.V.
dc.contributor.author Stepanov V.P.
dc.contributor.author Bogomolov E.S.
dc.contributor.author Levskii L.K.
dc.contributor.author Sergeev S.A.
dc.date.accessioned 2024-10-27T02:28:35Z
dc.date.available 2024-10-27T02:28:35Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=13514469
dc.identifier.citation Doklady Earth Sciences, 2006, 407, 2, 304-307
dc.identifier.issn 1028-334X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/46214
dc.description.abstract Determination of the age boundaries of magmatic activity and elucidation of the sequence of magmatic eruptions in certain magmatic provinces allow correlation of magmatic events over wide areas. This is of great importance for understanding the reasons and manner of evolution of deep magmatic processes. Kimberlites and lamproites were emplaced in the East European Craton (in particular, in the Baltic Shield and adjacent areas) in several stages. The Devonian stage was marked by the wide occurrence of alkaliultramafic rocks (including kimberlites) in the Baltic Shield (Kola Peninsula and Karelia), Arkhangelsk district, Middle Timan, and Ukrainian Shield (eastern Azov region).
dc.subject Baltic shield
dc.title TIMING AND DURATION OF KIMBERLITIC MAGMATISM IN THE ZIMNII BEREG DIAMONDIFEROUS PROVINCE: EVIDENCE FROM RB-SR AGE DATA ON KIMBERLITE SILLS ALONG THE MELA RIVER
dc.type Статья
dc.identifier.doi 10.1134/S1028334X06020346
dc.subject.age Палеозой::Девонская


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