The Age, Sources, and Tectonic Setting of Tin-Bearing Granites of the Yazovka Complex of the Baikal–Patom Fold-Thrust Belt

Granite–porphyries of the Yazovka complex occur in the northern part of the Riphean Baikal–Patom fold-thrust belt within the Tonod Uplift of the Early Precambrian basement. The geochronological (U–Pb), isotope-geochemical (Sm–Nd), and geochemical studies have shown that the rocks of this complex bel...

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Bibliographic Details
Published in:Doklady earth sciences 2020-02, Vol.490 (2), p.55-59
Main Authors: Larin, A. M., Kotov, A. B., Salnikova, E. B., Sklyarov, E. V., Kovach, V. P., Plotkina, Yu. V., Anisimova, I. V., Podolskaya, M. M.
Format: Article
Language:English
Subjects:
Earth and Environmental Science
Earth Sciences
Geochemistry
Geochronology
Geological time
Geology
Granite
Isotopes
Lava
Magma
Mantle
Precambrian
Tectonics
Tectonics (Geology)
Tin
Uplift
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Summary:Granite–porphyries of the Yazovka complex occur in the northern part of the Riphean Baikal–Patom fold-thrust belt within the Tonod Uplift of the Early Precambrian basement. The geochronological (U–Pb), isotope-geochemical (Sm–Nd), and geochemical studies have shown that the rocks of this complex belong to A-type tin-bearing granites of the age of 709 ± 7 Ma. Initial magma of these granites was formed from the mixed Early Precambrian crustal and mantle source in the intraplate geodynamic setting. This tectonic event was global in nature and manifested the Late Riphean impulse of the lithospheric extension, which was associated with breakup of the supercontinent Rodinia under the influence of a mantle superplume.
ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X20020075