GEOCHRONOLOGICAL BOUNDARIES AND GEODYNAMIC INTERPRETATION OF ALKALINE-MAFIC MAGMATISM IN KUZNETSK ALATAU

dc.contributor.author	Vrublevsky V.V.
dc.contributor.author	Gertner I.F.
dc.contributor.author	Voitenko D.N.
dc.contributor.author	Vladimirov A.G.
dc.contributor.author	Rudnev S.N.
dc.contributor.author	Borisov S.M.
dc.contributor.author	Levchenkov O.A.
dc.date.accessioned	2022-07-25T04:36:25Z
dc.date.available	2022-07-25T04:36:25Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13461982
dc.identifier.citation	Doklady Earth Sciences, 2004, 398, 7, 990-994
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38391
dc.description.abstract	The available geochronological data indicate three evolutionary stages of alkaline-mafic magmatism in Kuznetsk Alatau (Cambrian-Ordovician, Early-Late Silurian, and Silurian-Devonian boundaries). These data support the observations reported in [14, 15] and assume that Phanerozoic continental growth of the southwestern margin of Siberian continent (in present-day coordinates) occurred in a complex geodynamic setting involving suprasubduction and plume sources.
dc.title	GEOCHRONOLOGICAL BOUNDARIES AND GEODYNAMIC INTERPRETATION OF ALKALINE-MAFIC MAGMATISM IN KUZNETSK ALATAU
dc.type	Статья

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