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NEW DATA ON THE AGE AND COMPOSITION OF OPHIOLITES FROM THE KABAK-TAIGA MASSIF (GORNY ALTAI)

https://doi.org/10.5800/GT-2025-16-2-0814

EDN: GISVEG

Abstract

The combination of newly obtained geological, petrological and geochronological data on the rocks from the Kabak-Taiga ophiolite massif of the Gorny Altai and already published materials on similar characteristics of the ophiolites from Tuva allows us to conclude that an initial back-arc basin at the rear of the Tannuol island arc dates back to the Vendian – Middle Cambrian. Its formation lasted for about 70 million years. The fragments of the back-arc basin are confined to the Middle Paleozoic Charysh-Terekta-Ulagan-Sayan suture-shear zone, formed as a result of the subduction of the oceanic crust of the back-arc basin beneath the Vendian-Cambrian Tannuola island arc of the Paleoasian Ocean.

About the Authors

V. D. Zindobryi
Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences
Russian Federation

3 Academician Koptyug Ave, Novosibirsk 630090



M. M. Buslov
Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences
Russian Federation

3 Academician Koptyug Ave, Novosibirsk 630090



A. V. Kotlyarov
Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences
Russian Federation

3 Academician Koptyug Ave, Novosibirsk 630090



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For citations:


Zindobryi V.D., Buslov M.M., Kotlyarov A.V. NEW DATA ON THE AGE AND COMPOSITION OF OPHIOLITES FROM THE KABAK-TAIGA MASSIF (GORNY ALTAI). Geodynamics & Tectonophysics. 2025;16(2):0814. (In Russ.) https://doi.org/10.5800/GT-2025-16-2-0814. EDN: GISVEG

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