Sand deposits in the Tokko basin of the Baikal rift zone: sources and provenance areas

作者: Skovitina T.M.¹, Kotov A.B.², Buchnev I.N.², Kovach V.P.², Velikoslavinskii S.D.², Tolmacheva E.V.², Adamskaya E.V.², Bobrovskaya O.V.³, Gorovoy V.A.¹
隶属关系:
1. Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences
2. Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences
3. St. Petersburg University
期: 卷 517, 编号 1 (2024)
页面: 21-26
栏目: GEOLOGY
##submission.dateSubmitted##: 31.01.2025
##submission.datePublished##: 13.12.2024
URL: https://rjmseer.com/2686-7397/article/view/649998
DOI: https://doi.org/10.31857/S2686739724070034
ID: 649998

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详细

The paper presents the results of U-Th-Pb (LA-ICP-MS) geochronological studies of detrital zircon from Quaternary sands of the Tokko basin on the eastern flank of the Baikal rift zone. The study shows, that their main sources were Mesoarchean tonalite-trondhjemite orthogneisses and metavolcanics, as well as Meso- and Neoarchean syn- and post-collision granitoids of the Charа-Olekma geoblock of the Aldan shield, which are located near the Tokko basin. Moreover, the supply of sedimentary material into it could have occurred during the melting of glaciers that covered the Udokan Uplift in the south and the Kodar Uplift in the north in the Middle-Late Quaternary.

关键词

sand deposits, detrital zircon, geochronology, Tokko basin, Baikal rift zone

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作者简介

T. Skovitina

Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences

编辑信件的主要联系方式.
Email: tatiana_skovitina@mail.ru
俄罗斯联邦, Irkutsk

A. Kotov

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: tatiana_skovitina@mail.ru

Corresponding Member of the RAS

俄罗斯联邦, St. Petersburg

I. Buchnev

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: tatiana_skovitina@mail.ru
俄罗斯联邦, St. Petersburg

V. Kovach

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: tatiana_skovitina@mail.ru
俄罗斯联邦, St. Petersburg

S. Velikoslavinskii

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: tatiana_skovitina@mail.ru
俄罗斯联邦, St. Petersburg

E. Tolmacheva

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: tatiana_skovitina@mail.ru
俄罗斯联邦, St. Petersburg

E. Adamskaya

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: tatiana_skovitina@mail.ru
俄罗斯联邦, St. Petersburg

O. Bobrovskaya

St. Petersburg University

Email: tatiana_skovitina@mail.ru
俄罗斯联邦, St. Petersburg

V. Gorovoy

Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences

Email: tatiana_skovitina@mail.ru
俄罗斯联邦, Irkutsk

参考

Логачев Н. А., Антощенко-Оленев И. В., Базаров Д. Б., Галкин В. И., Голдырев Г. С., Ендрихинский А. С., Золоторев А. Г., Сизиков А. И., Уфимцев Г. Ф. Нагорья Прибайкалья и Забайкалья. М.: Наука, 1974. 359 с.
Солоненко В. П., Тресков А. А., Курушин Р. А., Мишарина Л. А. Павлов О. В., Пшенников К. В., Солоненко М. А., Фомина Е. В., Хилько С. Д. Живая тектоника, вулканы и сейсмичность Станового нагорья. М.: Наука, 1966. 231 с.
Имаева Л. П., Мельникова В. И., Имаев В. С., Козьмин Б. М., Мельников А. И. Эволюция сейсмотектонических процессов восточного фланга Байкальской рифтовой зоны. Иркутск: Институт земной коры СО РАН, 2012. 170 с.
Замараев С. М., Васильев Е. П., Мазукабзов А. М., Ружич В. В., Рязанов Г. В. Соотношение древней и кайнозойской структур в Байкальской рифтовой зоне. Новосибирск: Наука, 1979. 126 с.
Геология и сейсмичность зоны БАМ. Структурно-вещественные комплексы и тектоника. Новосибирск: Наука, 1983. 189 с.
Логачев Н. А. История и геодинамика Байкальского рифта // Геология и геофизика. 2003. Т. 144. № 5. С. 510–513.
Jackson S. E., Pearson N. J., Griffin W. L., Belousova E. A. The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U–Pb zircon geochronology // Chem. Geol. 2004. V. 211. P. 47–69.
Horstwood M. S. A., Košler J., Gehrels G., Jackson S. E., McLean N. M., Paton Ch., Pearson N. J., Sircombe K., Sylvester P., Vermeesch P., Bowring J. F., Condon D. J., Schoene B. Community-Derived Standards for LA-ICP-MS U–(Th-)Pb Geochronology – Uncertainty Propagation, Age Interpretation and Data Reporting // Geostandards and Geoanalytical Research. 2016. V. 40. P. 311–332.
Van Achterbergh E., Ryan C. G., Jackson S. E., Griffin W. L. LA-ICP-MS in the Earth sciences – appendix 3, data reduction software for LA-ICP-MS / In: Sylvester P. J. (Ed.). St. John's, Canada: Short Course Mineralogical Assoc., 2001. V. 29. P. 239–243.
Andersen T. Correction of common lead in U–Pb analyses that do not report 204Pb // Chem. Geol. 2002. V. 192. P. 59–79.
Vermeesch P. IsoplotR: a free and open toolbox for geochronology // Geoscience Frontiers. 2018. V. 9. P. 1479–1493.
Gehrels G. E. Detrital zircon U-Pb geochronology: current methods and new opportunities. // In: Busby, C., Azor, A. (Eds.). Tectonics of Sedimentary Basins: Recent Advances. Chichester, UK: Wiley-Blackwell, 2012. P. 47–62.
Котов А. Б. Граничные условия геодинамических моделей формирования континентальной коры Алданского щита / Автореф. дис. … докт. геол.-мин. наук. СПб.: Изд-во СПбГУ, 2003. 78 с.
Kovach V., Adamskaya E., Kotov A., Podkovyrov V., Tolmacheva E., Gladkochub D., Sklyarov E., Velikoslavinsky S., Plotkina Y., Skovitina T., Wang K.-L., Lee H.-Y., Gorokhovsky B. Age of provenance for the Palaeoproterozoic Kemen Group, Udokan Complex: Newly recognised Palaeoproterozoic crust-forming event in the western Aldan Shield, Siberian Craton // Precambrian Research. 2023. 396. 107158.
Сковитина Т. М., Котов А. Б., Лопатин Д. В., Ковач В. П., Бучнев И. Н., Адамская Е. В., Бобровская О. В. Источники позднекайнозойских отложений эолового массива «Пески» Чарской впадины Байкальской рифтовой зоны: первые результаты U-Th-Pb (La-ICP-MS) геохронологических исследований детритового циркона // ДАН. Науки о Земле. 2023. Т. 510. № 1. С. 11–17.
Ковач В. П., Самсонов А. В., Котов А. Б., Сальникова Е. Б., Адамская Е. В., Бортников В. В., Степанова А. В., Ерофеева К. Г., Плоткина Ю. В., Федосеенко А. М., Сковитина Т.М. Аркозовые песчаники кебектинской серии Угуйского грабена (Алданский щит): возраст, источники и обстановки накопления // ДАН. Науки о Земле. 2023. Т. 512. № 1. С. 12–20.

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2. Fig. 1. Scheme of the geological structure of the western part of the Aldan Shield. 1 - Cenozoic plateau basalts (N2-Q); 2 - Cenozoic sandy deposits of rift basins; 3 - Mesozoic, Paleozoic and Neoproterozoic platform deposits; 4 - Phanerozoic granitoids; 5 - Paleoproterozoic granites of the Kodar complex; 6 - Paleoproterozoic metasedimentary rocks of the Udokan series; 7 - weakly metamorphosed sedimentary and volcanic rocks of the Mesoarchean greenstone belts of the Subgana complex; 8 - Meso- and Paleorcean tonalite-trondhjemite orthogneisses and Mesoarchean intrusive granitoids of the Charo-Olkma geoblock of the Aldan Shield; 9 – junction zone of the Aldan Shield and the Central Asian mobile belt (Stanovoy structural suture); 10 – Selenga-Stanovoy superterrane of the Central Asian mobile belt; 11 – Baikal-Patom region; 12 – faults; 13 – sampling sites for geochronological studies and their numbers. Roman numerals indicate: I – Chara Depression, II – Tokka Depression, III – Uguy Graben.

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3. Fig. 2. Distribution histograms and relative probability curves of the ages of detrital zircon from the Quaternary sands of the Tokka Depression (samples STM-32 and STM-33).

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