gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2024-15-5-0779WGKVZXgtcrust-1915Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSАМФИБОЛ-ФЛОГОПИТСОДЕРЖАЩИЕ КСЕНОЛИТЫ ИЗ КИМБЕРЛИТОВ КАК СВИДЕТЕЛЬСТВО МЕТАСОМАТИЧЕСКИХ ПРОЦЕССОВ В ЛИТОСФЕРНОЙ МАНТИИ ПОД КУОЙКСКИМ КИМБЕРЛИТОВЫМ ПОЛЕМAMPHIBOLE-PHLOGOPITE XENOLITHS FROM KIMBERLITES AS EVIDENCE OF METASOMATIC PROCESSES IN THE LITHOSPHERIC MANTLE BENEATH KUOIKA FIELDhttps://orcid.org/0000-0002-9808-6513КалашниковаТ. В.KalashnikovaT. V.

664033, Иркутск, ул. Фаворского, 1а

664033, Иркутск, ул. Лермонтова, 128 

1а Favorsky St, Irkutsk 664033 

128 Lermontov St, Irkutsk 664033 

kalashnikova@igc.irk.ruhttps://orcid.org/0000-0001-9023-9362КостровицкийС. И.KostrovitskyS. I.

664033, Иркутск, ул. Фаворского, 1а

664033, Иркутск, ул. Лермонтова, 128 

1а Favorsky St, Irkutsk 664033 

128 Lermontov St, Irkutsk 664033 

https://orcid.org/0000-0001-9608-3602ДымшицА. М.DymshitsA. M.

664033, Иркутск, ул. Лермонтова, 128

128 Lermontov St, Irkutsk 664033

Институт геохимии им. А.П. Виноградова СО РАН ; Институт земной коры СО РАНРоссияVinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of Sciences ; Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of SciencesRussian FederationИнститут земной коры СО РАНРоссияInstitute of the Earth’s Crust, Siberian Branch of the Russian Academy of SciencesRussian Federation202418102024155779779Copyright © Калашникова Т.В., Костровицкий С.И., Дымшиц А.М., 20242024Калашникова Т.В., Костровицкий С.И., Дымшиц А.М.Kalashnikova T.V., Kostrovitsky S.I., Dymshits A.M.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/1915

В работе впервые приводятся данные по содержанию редких элементов в минералах из пород с признаками модальных метасоматических изменений из кимберлитовой трубки Обнаженной, которые сравниваются с ксенолитами из данной трубки без признаков модального метасоматоза. На основании содержания редких элементов в клинопироксене и амфиболе, а также 40Ar/39Ar датирования флогопита делается вывод о том, что в нижнем протерозое в литосферной мантии под Куойкским кимберлитовым полем образовывались расплавы-флюиды, обогащенные Nb+Ta, а также редкими землями, которые приводили к развитию флогопит-амфиболовой минерализации по пироксену.

This paper devoted to the mantle xenoliths with evidence of modal metasomatic alteration from the Obnazhennaya kimberlite pipe (Kuoika kimberlite field). The first data presents for trace elements content in minerals from such rocks, and they are compared with xenoliths from this pipe having no evidence of modal metasomatism. Based on the trace elements content in clinopyroxene and amphibole, as well as 40Ar/39Ar dating of phlogopite, it was concluded that enriched in Nb+Ta and REE melt-fluids were formed beneath the Kuoika field in the Lower Proterozoic, which lead to the phlogopite-amphibole formation from pyroxene.

амфиболфлогопитлитосферная мантияметасоматизмСибирский кратонamphibolephlogopitelithospheric mantlemetasomatismSiberian cratonИсследование выполнено за счет гранта РНФ (проект № 22-77-10073 «Реконструкция термального режима и состава литосферной мантии Сибирского кратона в районах проявления кимберлитового магматизма») (определены редкоэлементные составы минералов).This research was funded by the Russian Science Foundation (project 22-77-10073 "Reconstruction of the thermal state and composition of the lithospheric mantle beneath the kimberlite fields of the Siberian craton") (traceelement mineral composition).ReferencesAgashev A.M., Ionov D.A., Pokhilenko N.P., Golovin A.V., Cherepanova Yu., Sharygin I.S., 2013. Metasomatism in Lithospheric Mantle Roots: Constraints from Whole-Rock and Mineral Chemical Composition of Deformed Peridotite Xenoliths from Kimberlite Pipe Udachnaya. 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The authors declare that there are no conflicts of interest present.