gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2019-10-2-0412gtcrust-839Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSМАНТИЙНЫЕ ТЕРРЕЙНЫ СИБИРСКОГО КРАТОНА: ИХ ВЗАИМОДЕЙСТВИЕ С ПЛЮМОВЫМИ РАСПЛАВАМИ НА ОСНОВАНИИ ТЕРМОБАРОМЕТРИИ И ГЕОХИМИИ МАНТИЙНЫХ КСЕНОКРИСТОВMANTLE TERRANES OF THE SIBERIAN CRATON: THEIR INTERACTION WITH PLUME MELTS BASED ON THERMOBAROMETRY AND GEOCHEMISTRY OF MANTLE XENOCRYSTShttps://orcid.org/0000-0003-3985-7661АщепковИ. В.AshchepkovI. V.

Игорь Викторович Ащепков - кандидат геоллого-минералогических наук, старший научный сотрудник

630090, Новосибирск, пр. Академика Коптюга, 3

Igor V. Ashchepkov - Candidate of Geology and Mineralogy, Senior Researcher

3 Academician Koptyug ave., Novosibirsk 630090

igor.ashchepkov@igm.nsc.ruИвановА. С.IvanovA. S.

678174, Мирный, Чернышевское шоссе, 16

Aleksandr S. Ivanov - Lead Researcher

16 Chernychevskoe highway, Mirny 678174

IvanovAS@alrosa.ruКостровицкийС. И.KostrovitskyS. I.

Сергей Иванович Костровицкий - доктор геолого-минералогических наук, ведущий научный сотрудник

664033, Иркутск, ул. Фаворского, 1А, 

664033, Иркутск, ул. Лермонтова, 128

Sergei I. Kostrovitsky - Doctor of Geology and Mineralogy, Lead Researcher

1A Favorsky street, Irkutsk 664033, 

128 Lermontov street, Irkutsk 664033

serkost@igc.irk.ruВавиловМ. А.VavilovM. A.

Михаил Анатольевич Вавилов - ведущий инженер

630090, Новосибирск, пр. Академика Коптюга, 3

Mikhail A. Vavilov - Lead Engineer

3 Academician Koptyug ave., Novosibirsk 630090

mav@igm.nsc.ruhttps://orcid.org/0000-0002-4806-7744БабушкинаС. А.BabushkinaS. A.

Светлана Анатольевна Бабушкина - кандидат геолого-минералогических наук, старший научный сотрудник

677007, Республика Саха (Якутия), Якутск, пр. Ленина, 39, 

677000, Республика Саха (Якутия), Якутск, ул. Белинского, 58

Svetlana A. Babushkina - Candidate of Geology and Mineralogy, Senior Researcher

39 Lenin avenue, Yakutsk 677007, Sakha (Yakutia) Republic, 

58 Belinsky street, Yakutsk 677000, Sakha (Yakutia) Republic

sa.babushkina@s-vfu.ruВладыкинН. В.VladykinN. V.

Николай Васильевич Владыкин - доктор геолого-минералогических наук

664033, Иркутск, ул. Фаворского, 1А

Nikolai V. Vladykin - Doctor of Geology and Mineralogy

1A Favorsky street, Irkutsk 664033

 

vlad@igc.irk.ruТычковН. С.TychkovN. S.

Николай Сергеевич Тычков - кандидат геолого-минералогических наук, старший научный сотрудник, заведующий лабораторией

630090, Новосибирск, пр. Академика Коптюга, 3

Nikolai S. Tychkov - Candidate of Geology and Mineralogy, Senior Researcher, Head of Laboratory

3 Academician Koptyug ave., Novosibirsk 630090

tych@igm.nsc.ruhttps://orcid.org/0000-0003-2783-071XМедведевН. С.MedvedevN. S.

Николай Сергеевич Медведев - кандидат химических наук

630090, Новосибирск, пр. Академика Лаврентьева, 3

Nikolai S. Medvedev Candidate of Chemistry

3 Academician Lavrentiev ave., Novosibirsk 630090

medvedev@niic.nsc.ruИнститут геологии и минералогии им. В.С. Соболева СО РАНРоссияV.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RASRussian FederationНаучно‐исследовательское геологоразведочное предприятие АК «АЛРОСА» (ПАО)РоссияGeological Enterprise of Exploration, Public Joint Stock Company «ALROSA»Russian FederationИнститут геохимии им. А.П. Виноградова СО РАН; Институт земной коры СО РАНРоссияA.P. Vinogradov Institute of Geochemistry, Siberian Branch of RAS; Institute of the Earth's Crust, Siberian Branch of RASRussian FederationИнститут геологии алмаза и благородных металлов СО РАН; Северо‐Восточный федеральный университет им. М.К. АммосоваРоссияInstitute of Diamond and Precious Metals Geology, Siberian Branch of RAS; M.K. Ammosov North‐Eastern Federal UniversityRussian FederationИнститут геохимии им. А.П. Виноградова СО РАНРоссияA.P. Vinogradov Institute of Geochemistry, Siberian Branch of RASRussian FederationИнститут неорганической химии им. А.В. Николаева СО РАНРоссияA.V. Nikolaev Institute of Inorganic Chemistry, Siberian Branch of RASRussian Federation201922062019102197245Copyright © Ащепков И.В., Иванов А.С., Костровицкий С.И., Вавилов М.А., Бабушкина С.А., Владыкин Н.В., Тычков Н.С., Медведев Н.С., 20192019Ащепков И.В., Иванов А.С., Костровицкий С.И., Вавилов М.А., Бабушкина С.А., Владыкин Н.В., Тычков Н.С., Медведев Н.С.Ashchepkov I.V., Ivanov A.S., Kostrovitsky S.I., Vavilov M.A., Babushkina S.A., Vladykin N.V., Tychkov N.S., Medvedev N.S.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/839

Вариации структуры и состава минералов из трубок Якутской кимберлитовой провинции (ЯКП) разных мантийных террейнов Сибирского кратона изучены с использованием обширной базы данных микрозондовых анализов минералов коллектива авторов (ИГМ, ИГХ, ИЗК и ИГБМ СО РАН и «АЛРОСА»), а также геохимических анализов минералов, выполненных методом индуктивно связанной масс‐спектрометрии c лазерной абляцией. Реконструирована слоистость под трубками, образованная 6– пластинами вероятного субдукционного генезиса, разделенными пироксенитовыми, эклогитовыми, метасоматическими горизонтами и линзами дунитов. Построены мантийные разрезы через кимберлитовые поля и протяженные трансекты. В пределах установленных тектонических террейнов предполагается коллаж из микроплит, возникших в раннем –среднем архее, а протяженные субмеридиональные структуры тектонических террейнов не всегда подтверждаются на мантийном уровне. Под Анабарским и Алданским щитами мантийные разрезы более грубослоисты и состоят из 3– крупных горизонтов дунитов с гнездами граната и пироксенов, разделенных ильменит‐флогопитовыми метасоматитами и пироксенитами. Террейны, представляющие шовные зоны между протократонами, как Хапчанский, часто насыщены эклогитами и пироксенитами, которые могут быть протяженными восходящими телами магматических эклогитов, прорывающих структуру мантийной лито‐ сферы (МЛ). Почти повсеместный пироксенитовый слой на уровне 3.5–.5 ГПа, вероятно, возник в раннем архее при высоком тепловом потоке при плавлении эклогитов и в дальнейшем трассировался плюмовыми расплавами. В пределах раннеархейских протократонов: гранит‐зеленокаменных террейнов –Тунгусского, Мархинского, Беректинского, Шарыжалгайского –с возрастом ~3.8–.0 млрд лет [Gladkochub et al., 2019] ман‐ тийная литосфера менее истощена и часто метасоматизирована. Далдынский и Маганский гранулит‐орто‐ гнейсовый террейны имеют слоистую структуру МЛ со складчатостью, проявленной в разрезах с севера на юг от тр. Удачной до тр. Краснопресненской и менее выраженной в широтном направлении. От Далдынского до Алакитского поля растет степень метасоматоза, щелочность пироксенов и количество флогопита. Наиболее продуктивные трубки Айхал и Юбилейная приурочены к дунитовому ядру, что сопровождается сменой специализации высокозарядных элементов Ta‐Nb на Zr‐Hf. В пределах Маганского террейна тонкослоистая структура средней и верхней части киля кратона сменяется резко истощенным продуктивным горизонтом в его основании. Мантия гранит‐зеленокаменного Мархинского террейна содержит горизонты эклогитов (часто пелитового типа), предполагающих субдукцию континентальной литосферы или осадков. В центральной и северной части Сибирского кратона в мантии преобладают структуры погружения на запад с небольшим углом. Рассмотрены особенности геохимии гранатов и пироксенов различных мантийных террейнов.

We have studied variations in the structure and composition of minerals from the pipes of the Yakutian kimberlite province (YKP) in different mantle terranes of the Siberian craton. The study was based on an extensive database, including the microprobe analysis datasets consolidated by IGM, IG, IEC and IGDNM SB RAS and ALROSA and geochemical analysis of minerals performed by LA‐ICP‐MS (Laser Ablation Inductively Coupled Plasma Mass Spectrometry). The reconstruction shows layering under the tubes, including 6–7 slab that were probably formed due to subduction; the slabs are separated by pyroxenitic, eclogitic and metasomatic layers and dunite lenses. Transects and mantle profiles across kimberlite fields are constructed. Within the limits of the revealed tectonic terranes, we assume a collage of microplates formed in the early – middle Archean. Extended submeridional structures of the tectonic terranes are not always confirmed at the mantle level. Beneath the Anabar and Aldan shields, the mantle sections show more coarse layers and 3–4 large horizons of dunites with garnet and pyroxene nests separated by ilmenite‐ phlogopite metasomatites and pyroxenites. Terranes representing the suture zones between the protocratons (e.g. Khapchan) are often saturated with eclogites and pyroxenites that may occur as leghthy ascending bodies of magmatic eclogites penetrating through the mantle lithosphere structure (ML). A nearly ubiquitous pyroxenite layer at the level of 3.5–4.5 GPa formed probably in the early Archean with a high heat flux during melting of eclogites and was subsequently traced by plume melts. Within the early Archean protocratons – granite‐greenstone terranes (Tungus, Markha, Berekta, and Sharyzhalgai, ~3.8–3.0 Gyr [Gladkochub et al., 2019], the mantle lithosphere is less depleted and largely metasomatized. The ML structure of the Daldyn and Magan granulite‐orthogneiss terranes is layered with folding revealed in the north‐to‐south sections from the Udachnaya pipe to the Krasnopresnenskaya pipe, which is less pronounced in the latitudinal direction. From the Daldyn field to the Alakit field, there is an increase in the degree of metasomatism, and higher alkalinity of pyroxenes and larger amounts of phlogopite are noted. The most productive Aikhal and Yubileinaya pipes are confined to a dunite core, which is accompanied by a change in the specialization of high‐charge elements Ta‐Nb to Zr‐Hf. Within the limits of the Magan terrane, the thin‐layer structure of the middle and upper parts of the craton keel is replaced with a sharply depleted productive horizon at its base. The mantle of the granite‐greenstone Markha terrrein comprises eclogite (often pelitic) horizons, which suggests subduction of the continental lithosphere or sediments. In the central and northern parts of the Siberian craton, most structures in the mantle are sinking to the west at small angles. The geochemistry features of garnets and pyroxenes from various mantle terranes are considered in detail.

мантийная литосфератеррейнСибирский кратонтермобарометрияперидотитыэклогитыгранатыкимберлитытрансектгеохимия редких элементовслоистостьокислительный потенциалплюмвзаимодействиеmantle lithosphereterraneSiberian cratonthermobarometryperidotiteeclogitegarnetkimberlitetransectgeochemistry of rare elementsstratification/layeringoxidative potentialplumeinteractionРабота выполнена при поддержке РФФИ (проект № 19‐05‐00788) и по государственному заданию ИГМ СО РАН (г. Новосибирск), а также НИГП АК «Алроса» ПАО (г. Якутск), ИГХ СО РАН (г. Иркутск), ИГАБМ СО РАН (г. Якутск) и ИЗК СО РАН (г. Иркутск)ReferencesAfanasiev V.P., Ashchepkov I.V., Verzhak V.V., O’Brien H., Palessky S.V., 2013. PT conditions and trace element variations of picroilmenites and pyropes from placers and kimberlites in the Arkhangelsk region, NW Russia. Journal of Asian Earth Sciences 70–71, 45–63. https://doi.org/10.1016/j.jseaes.2013.03.002.Afanasiev V.P., Ashchepkov I.V., Verzhak V.V., O’Brien H., Palessky S.V., 2013. 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The authors declare that there are no conflicts of interest present.