gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2023-14-6-0729gtcrust-1759Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSМОДЕЛЬ ТЕРМОТЕКТОНИЧЕСКОЙ ЭВОЛЮЦИИ ПОРОД ДОМЕЗОЗОЙСКОГО ФУНДАМЕНТА ЮЖНОЙ ТУВЫ В ПОЗДНЕМ МЕЗОЗОЕ И КАЙНОЗОЕA MODEL OF THE LATE MESOZOIC AND CENOZOIC THERMOTECTONIC EVOLUTION OF THE PRE-MESOZOIC BASEMENT ROCKS IN SOUTH TUVAВетровЕ. В.VetrovE. V.

630090, Новосибирск, пр-т Академика Коптюга, 3

3 Academician Koptyug Ave, Novosibirsk 630090

ВетроваН. И.VetrovaN. I.

630090, Новосибирск, пр-т Академика Коптюга, 3

3 Academician Koptyug Ave, Novosibirsk 630090

Институт геологии и минералогии им. В.С. Соболева СО РАНРоссияSobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of SciencesRussian Federation202314122023146729729Copyright © Ветров Е.В., Ветрова Н.И., 20232023Ветров Е.В., Ветрова Н.И.Vetrov E.V., Vetrova N.I.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/1759

Выполнено термотектоническое моделирование на основе данных трекового анализа апатита для кристаллических пород Южной Тувы. Термотектоническое моделирование позволило визуализировать историю охлаждения пород домезозойского фундамента в позднемезозойское и кайнозойское время, восстановить хронологию и масштаб денудационных процессов за последние 125 млн лет и реконструировать эволюцию палеорельефа Южной Тувы за последние 100 млн лет. Результаты моделирования демонстрируют несколько мезозойско-кайнозойских эпизодов охлаждения, связанных с дифференцированной денудацией и эксгумацией пород домезозойского фундамента. Неравномерная денудация связана с асинхронной активизацией разломных структур, контролирующих тектоническую эволюцию Южной Тувы. Показано, что раннемеловая (~125–100 млн лет) активизация Агардакско-Окинской надвиговой зоны могла произойти в результате постколлизионных процессов после столкновения Сибири и Амурии и/или последовательной коллизии между киммерийскими блоками. Усиленная активизация Агардакско-Окинской разломной зоны, сопровождаемая значительной эксгумацией пород восточной части фундамента Южной Тувы до абсолютных отметок 1200 м, в позднем мелу (~100–75 млн лет) могла быть вызвана Каракорамско-Памирской коллизией на юге Евразии. Активизация главных разломных зон Южной Тувы в позднем кайнозое (25–0 млн лет) является эффектом дальнего воздействия от Индо-Евразийской коллизии в южной части Евразийского континента. В это время произошло максимальное поднятие фундамента в зоне сочленения Южно-Таннуольской и Убсунур-Бийхемской разломных зон и трансформация рельефа Южной Тувы от среднерасчлененного с абсолютными высотами от 500 до 1400 м до современного с абсолютными высотами от 800 до 2600 м.

Thermotectonic modeling was performed for the crystalline rocks of South Tuva using the apatite fission-track analysis. Thermotectonic modeling made it possible to visualize the Late Mesozoic and Cenozoic cooling history of the Pre-Mesozoic basement rocks, and to reconstruct the chronology and scale of the denudational processes over the last 125 myr and the evolution of paleorelief of South Tuva over the last 100 myr. The modeling results depicted several Mesozoic-Cenozoic episodes of cooling due to differential denudation and exhumation of the Pre-Mesozoic basement rocks. A differential denudation is related to an asynchronous activation of fault structures controlling the tectonic evolution of South Tuva. It is shown that the Early Cretaceous (~125–100 Ma) activation of the Agar-Dag-Oka thrust fault zone could result from the post-collisional processes after the collision between Siberia and Amuria and/or consecutive collision between the Cimmerian blocks. An intense activation of the Agar-Dag-Oka fault zone in the Late Cretaceous (~100–75 Ma), accompanied by significant basement rock exhumation in the eastern South Tuva to absolute heights of 1200 m, could be caused by the Karakoram-Pamir collision in the south of Eurasia. The Late Cenozoic (25–0 Ma) activation of the main fault zones of South Tuva represents a far-field effect of the Indo-European collision on the southern Eurasian continent. At the same time, there were the maximum basement uplift in the junction zone between the South Tannuola and Ubsunur-Bii-Khem fault zones and the transformation of relief of South Tuva from moderately dissected, with absolute heights of 500 to 1400 m, to modern, with absolute heights of 800 to 2600 m.

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The authors declare that there are no conflicts of interest present.