gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2025-16-6-0859TJNZRNgtcrust-2150Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSГЕОДИНАМИЧЕСКИЕ УСЛОВИЯ СЕДИМЕНТАЦИИ И ИСТОЧНИКИ ПАЛЕОЗОЙСКИХ ТЕРРИГЕННЫХ ОТЛОЖЕНИЙ ЯМКУНСКОЙ СЕРИИ АРГУНСКОГО КОНТИНЕНТАЛЬНОГО МАССИВАGEODYNAMIC CONDITIONS OF SEDIMENTATION AND SOURCES OF PALEOZOIC TERRIGENOUS ROCKS FROM THE YAMKUN SERIES OF THE ARGUN CONTINENTAL MASSIFhttps://orcid.org/0000-0001-5221-5140СмирноваЮ. Н.SmirnovaYu. N.

675000, Благовещенск, пер. Релочный, 1

1 Relochniy ln, Blagoveshchensk 675000

smirnova@ascnet.ruhttps://orcid.org/0000-0001-5460-2769КуриленкоА. В.KurilenkoA. V.

199106, Санкт-Петербург, пр-т Средний, 74

670047, Улан-Удэ, ул. Сахьяновой, 6а, Республика Бурятия

74 Sredny Ave, Saint Petersburg, 199106

6а Sakhyanova St, Ulan-Ude 670047, Republic of Buryatia

Институт геологии и природопользования ДВО РАНРоссияInstitute of Geology and Nature Management, Far Eastern Branch of the Russian Academy of SciencesRussian FederationВсероссийский научно-исследовательский геологический институт им. А.П. Карпинского ; Геологический институт им. Н.Л. Добрецова СО РАНРоссияKarpinsky Russian Geological Research Institute ; Dobretsov Geological Institute, Siberian Branch of the Russian Academy of SciencesRussian Federation202511122025166859859Copyright © Смирнова Ю.Н., Куриленко А.В., 20252025Смирнова Ю.Н., Куриленко А.В.Smirnova Y.N., Kurilenko A.V.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/2150

В публикации приведены особенности распределения основных породообразующих компонентов и микроэлементов в палеозойских терригенных отложениях ильдиканской и газимурозаводской свит ямкунской серии Аргунского континентального массива. Главной целью исследований является реконструкция обстановок накопления и определение основных источников кластического материала. Показано, что терригенные породы ильдиканской и газимурозаводской свит соответствуют различным литотипам: грауваккам, аркозам и литоидным аренитам. Согласно вариациям величин Zr/Sc и Th/Sc отложения ямкунской серии являются породами первого цикла седиментации. Анализ геохимического состава изученных пород свидетельствуют о том, что основными источниками кластического материала для них являлись кислые и средние магматические породы при возможном вовлечении в осадконакопление пород основного состава. Эти данные в совокупности с результатами U-Pb геохронологических исследований магматических образований Аргунского массива позволяют предполагать, что основными источниками исходного материала являлись тонийские, кембрийские, ордовикские и раннесилурийские магматические породы кислого и среднего состава, широко распространенные в пределах Аргунского континентального массива. В качестве дополнительных источников сноса стоит рассматривать палеопротерозойские ортогнейсы комплекса Синхуадукоу Аргунского массива. В свою очередь, положение фигуративных точек состава палеозойских терригенных отложений ямкунской серии Аргунского массива на тектонических дискриминационных диаграммах, а также накопленные геологические данные свидетельствуют о формировании нижне- и среднедевонских отложений ильдиканской свиты в обстановке пассивной континентальной окраины, а нижнекаменноугольных пород газимурозаводской свиты – в обстановке активной континентальной окраины или островной дуги.

The paper deals with the distribution of the major oxides and trace elements in the Paleozoic terrigenous rocks of the Ildikan and Gazimursky Zavod formations from the Yamkun series of the Argun continental massif. The main purpose of the study is to reconstruct depositional settings and sources of clastic material. It is shown that the terrigenous rocks of the Ildikan and Gazimursky Zavod formations correspond to different lithotypes: graywackes, arkoses, and litharenites. According to the variations in Zr/Sc and Th/Sc ratios, the rocks of the Yamkun series are the first-cycle sediments. Whole-rock geochemical composition of studied rocks suggests that the main sources of clastic material were felsic and intermediate igneous rocks, with a subordinate amount of mafic rocks. The use of these data in combination with the U-Pb geochronological data on igneous rocks from the Argun massif implies that the initial material was mainly sourced from the Tonian, Cambrian, Ordovician and Early Silurian felsic and intermediate igneous rocks, widely abundant within the Argun continental massif. Additional sources of clastic material may involve the Paleoproterozoic orthogneisses from the Xinhuadukou complex of the Argun massif. The position of figurative points of the composition of the Paleozoic terrigenous rocks from the Yamkun series of the Argun massif on the tectonic discriminant diagrams in combination with geological data indicates a passive continental margin setting for the Lower-Middle Devonian deposits of the Ildikan formation and an active continental margin (or island-arc) setting for the Lower Carboniferous deposits of the Gazimursky Zavod formation.

ильдиканская свитагазимурозаводская свитатерригенные породыпалеогеодинамикаАргунский массивIldikan formationGazimursky Zavod formationterrigenous rockspaleogeodynamicsArgun massifИсследование проведено в рамках госзадания ИГиП ДВО РАН (№ 122041800127-8, «Геодинамические обстановки, основные этапы тектонической эволюции и металлогения восточной части Центрально-Азиатского складчатого пояса»).The study was carried out on the state assignment of the Institute of Geology and Nature Management FEB RAS (No. 122041800127-8, "Geodynamic settings, main stages of tectonic evolution and metallogeny of the eastern part of the Central Asian Orogenic Belt").ReferencesBhatia M.R., 1983. Plate Tectonics and Geochemical Composition of Sandstones. Journal of Geology 91 (6), 611–627. https://doi.org/10.1086/628815.Bhatia M.R., 1983. Plate Tectonics and Geochemical Composition of Sandstones. Journal of Geology 91 (6), 611–627. https://doi.org/10.1086/628815.Bhatia M.R., Сrook K.A.W., 1986. 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The authors declare that there are no conflicts of interest present.