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

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Abstract

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.

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About the authors

T. M. Skovitina

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

Author for correspondence.
Email: tatiana_skovitina@mail.ru
Russian Federation, Irkutsk

A. B. Kotov

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: tatiana_skovitina@mail.ru

Corresponding Member of the RAS

Russian Federation, St. Petersburg

I. N. Buchnev

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: tatiana_skovitina@mail.ru
Russian Federation, St. Petersburg

V. P. Kovach

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: tatiana_skovitina@mail.ru
Russian Federation, St. Petersburg

S. D. Velikoslavinskii

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: tatiana_skovitina@mail.ru
Russian Federation, St. Petersburg

E. V. Tolmacheva

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: tatiana_skovitina@mail.ru
Russian Federation, St. Petersburg

E. V. Adamskaya

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: tatiana_skovitina@mail.ru
Russian Federation, St. Petersburg

O. V. Bobrovskaya

St. Petersburg University

Email: tatiana_skovitina@mail.ru
Russian Federation, St. Petersburg

V. A. Gorovoy

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

Email: tatiana_skovitina@mail.ru
Russian Federation, Irkutsk

References

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Supplementary files

Supplementary Files
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1. JATS XML
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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