gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2024-15-5-0788CLVRWDgtcrust-1924Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSПАЛЕОЗОЙСКИЙ ВНУТРИПЛИТНЫЙ МАГМАТИЗМ ВОСТОЧНО-ЕВРОПЕЙСКОЙ ПЛАТФОРМЫ: СРАВНИТЕЛЬНЫЙ АНАЛИЗ ПРИПЯТСКО-ДНЕПРОВСКО-ДОНЕЦКОЙ РИФТОВОЙ ЗОНЫ И КОЛА-АРХАНГЕЛЬСКОЙ ПРОВИНЦИИPALEOZOIC INTRAPLATE MAGMATISM OF THE EAST EUROPEAN PLATFORM: COMPARATIVE ANALYSIS OF THE PRIPYAT-DNIEPER-DONETS RIFT ZONE AND THE KOLA-ARKHANGELSK PROVINCEhttps://orcid.org/0000-0003-0618-3656ЮткинаЕ. В.YutkinaE. V.

119017, Москва, пер. Старомонетный, 35

35 Staromonetny Ln, Moscow 119017

eyutkina@gmail.comhttps://orcid.org/0000-0002-7510-642XКаргинА. В.KarginA. V.

119017, Москва, пер. Старомонетный, 35

35 Staromonetny Ln, Moscow 119017

НосоваА. А.NosovaA. A.

119017, Москва, пер. Старомонетный, 35

35 Staromonetny Ln, Moscow 119017

КузьменковаО. Ф.KuzmenkovaO. F.

220084, Минск, ул. Академика Купревича, 7

7 Akademika Kuprevicha St, 220084 Minsk

СазоноваЛ. В.SazonovaL. V.

119017, Москва, пер. Старомонетный, 35

119991, Москва, Ленинские горы, 1

35 Staromonetny Ln, Moscow 119017

1 Leninskie Gory, Moscow 119991

https://orcid.org/0000-0003-2112-681XКондрашовИ. А.KondrashovI. A.

119017, Москва, пер. Старомонетный, 35

35 Staromonetny Ln, Moscow 119017

Институт геологии рудных месторождений, петрографии, минералогии и геохимии РАНРоссияInstitute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry, Russian Academy of SciencesRussian FederationНПЦ по геологииБеларусьNPC for GeologyBelarusИнститут геологии рудных месторождений, петрографии, минералогии и геохимии РАН ; Московский государственный университет им. М.В. ЛомоносоваРоссияInstitute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry, Russian Academy of Sciences ; Lomonosov Moscow State UniversityRussian Federation202419102024155788788Copyright © Юткина Е.В., Каргин А.В., Носова А.А., Кузьменкова О.Ф., Сазонова Л.В., Кондрашов И.А., 20242024Юткина Е.В., Каргин А.В., Носова А.А., Кузьменкова О.Ф., Сазонова Л.В., Кондрашов И.А.Yutkina E.V., Kargin A.V., Nosova A.A., Kuzmenkova O.F., Sazonova L.V., Kondrashov I.A.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/1924

В статье приводится сравнение геохронологических, геохимических и Sr-Nd изотопных данных, а также анализ геодинамических условий проявления девонского магматизма Восточно-Европейской платформы на примере Припятско-Днепровско-Донецкой рифтовой зоны на юге платформы и Кола-Архангельской щелочной провинции на севере.

Позднепалеозойский рифтогенез юга платформы сопровождался магматизмом с образованием широкого спектра пород – от щелочно-ультраосновных лампрофиров и оранжеитов, неалмазоносных кимберлитов и карбонатитов до типичных толеитов, трахиандезитов и трахириодацитов. На севере платформы при активизации рифтов происходило формирование разнообразных по составу магматических проявлений с преобладанием кимберлитов, в том числе промышленно-алмазоносных (Архангельская алмазоносная провинция), что является основной отличительной особенностью этой провинции. Для Припятско-Днепровско-Донецкой рифтовой зоны была выявлена обратная латеральная геохимическая зональность источников – от деплетированной мантии в осевой зоне Днепровско-Донецкого прогиба к более обогащенной в краевых частях – плечах прогиба (Приазовье, Воронежский кристаллический массив): вдоль оси рифтовой зоны с юго-востока на северо-запад к Жлобинской седловине (оранжеиты, щелочные пикриты жлобинского щелочно-ультрамафитового комплекса) и в Припятском прогибе (припятский щелочной и субщелочной мафитовый комплекс), а также перпендикулярно оси от центральной части Днепровско-Донецкого прогиба на юго-запад к Восточному Приазовью (неалмазоносные кимберлиты) и на северо-восток к Воронежскому кристаллическому массиву.

Имеющиеся петролого-минералогические и изотопно-геохимические данные по магматитам обеих крупных магматических структур позволяют говорить о значительной степени гетерогенности литосферы, участии в формировании пород нескольких типов источников и о существенном влиянии коровой составляющей как в южной, так и в северной части Восточно-Европейской платформы.

This paper presents a comparative analysis of geochronological, geochemical, Sr-Nd isotopic data and geodynamic conditions for the Devonian magmatism of the East European Platform, using as an example the Pripyat-Dnieper-Donets rift zone in the south of the platform and the Kola alkaline province in the north.

The Late Paleozoic rifting in the south of the platform was accompanied by magmatism, which formed a wide range of rocks, from alkaline-ultramafic lamprophyres and orangeites, non-diamondiferous kimberlites and carbonatites to typical tholeiites, trachyandesites, and trachyrhyodacites. Activation of rifting processes in the north of the platform has also produced a compositional diversity of magmatic occurrences dominated by kimberlites, in particular diamondiferous (Arkhangelsk diamond-bearing province), which is the main distinctive feature of the place. The Pripyat-Dnieper-Donets rift zone is subject to reverse lateral geochemical zonality of the mantle sources – from those depleted in the axial zone of the Dnieper-Donets trough to more enriched in the marginal parts – trough shoulders (Azov region, Voronezh crystalline massif): along the southeast to northwest axis of the rift zone to the Zhlobin saddle (orangeites, alkaline picrites of the Zhlobin alkaline-ultramafic complex) and in the Pripyat trough (Pripyat alkaline and subalkaline mafic complex) as well was perpendicular to the axis from the central part of the Dnieper-Donets trough to the southwest towards the Eastern Azov region (non-diamondiferous kimberlites) and to the northeast towards the Voronezh crystalline massif.

Currently available petrological-mineralogical and isotopic-geochemical data on magmatites of both large magmatic structures suggest significant lithospheric heterogeneity, different types of sources of formation of rocks, and a significant influence exerted by the crustal component both in the southern and northern parts of the East European platform.

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The authors declare that there are no conflicts of interest present.