Инд. авторы:	Vetrov E.V., Kotler P.D., Kruk N.N., Zhigalov S.V., Babin G.A., Fedoseev G.S., Vetrova N.I.
Заглавие:	Evolution of the Kolyvan-Tomsk granitoid magmatism (Central Siberia): Insights into the tectonic transition from post-collision to intraplate settings in the northwestern part of the Central Asian Orogenic Belt
Библ. ссылка:	Vetrov E.V., Kotler P.D., Kruk N.N., Zhigalov S.V., Babin G.A., Fedoseev G.S., Vetrova N.I. Evolution of the Kolyvan-Tomsk granitoid magmatism (Central Siberia): Insights into the tectonic transition from post-collision to intraplate settings in the northwestern part of the Central Asian Orogenic Belt // Gondwana Research. - 2021. - Vol.93. - P.26-47. - ISSN 1342-937X. - EISSN 1878-0571.
Идентиф-ры:	DOI: 10.1016/j.gr.2021.01.008; РИНЦ: 44978105; WoS: 000634524600002;
Реферат:	eng: Late Paleozoic - earlyMesozoic geological evolution of the Kolyvan-Tomsk Fold Zone (KTFZ) located in the northwestern part of the Central Asian Orogenic Belt is significant to understanding the tectonic transition from postcollision to intraplate settings. We present new whole-rock geochemical and Sr-Nd isotopic data, and in situ zircon U-Pb ages for granitic rocks from the KTFZ basement to constrain their petrogenesis and to characterize changing of the tectonic setting and geodynamic evolution. Zircon U-Pb ages reveal extended multi-stage emplacement of the KTFZ granitoids for about 20 Ma from similar to 260 to similar to 240 Ma, that can be divided into two stages: the Permian-Triassic (similar to 260 to 250 Ma) and the Triassic (similar to 250 to 240 Ma). The Permian -Triassic granitic rocks with SiO2 between 63% and 74% have high LREE, HFSE (except Nb and Ta), Sr, Mg#, Cr, Ni concentrations, Sr/Y and (La/Yb)(N) ratios and remarkably low Y and Yb contents and Sr-87/Sr-86((T)) values (0.704682 and 0.703368). They are magnesian and show metaluminous to weakly peraluminous natures, indicating their formation through high degree fractionation of mantle-derived magmas. The Triassic granitoids exhibit extremely high SiO2 (73-77%), HFSE, HREE, Rb contents, Rb/Sr ratios and elevated negative Eu and Sr anomalies, low Mg#. They are ferroan and have a peraluminous nature with the absence of aluminium-rich minerals, all of which indicate the presence of the crustal substance in the magma source. Isotopic Nd compositions show that the both the Permian -Triassic and Triassic granitoids have uniform magma's, whichwere derived frompartialmelting of juvenile Neoproterozoic sources. These two stages of granitoid magmatism are interpreted as reflecting the transition from post-collisional magmatism, related to the final closure of the Paleo-Asian Ocean due to collision between the Baltica and Siberian paleocontinents during the Late Permian - Early Triassic and hence, to the intraplatemagmatism. The formation of the KTFZ granitic rocks was induced by an upwelling asthenosphere in an extensional geodynamic setting. During the post-collisional process, the large-scale lithospheric delamination plays a key role in the genesis of the Permian-Triassic granitoids and provide the magma generation for them. In the Triassic, we propose additional source of heat from mantle plume beneath the KTFZ, which promote extending of the granitoid magmatism in intraplate setting. (C) 2021 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
Ключевые слова:	Sr-Nd isotopes; Zircon U-Pb dating; Post-collisional; Kolyvan-Tomsk Fold Zone; Intraplate; Central Asian Orogenic Belt;
Издано:	2021
Физ. хар-ка:	с.26-47
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