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Czech Academy of Sciences, Institute of Geology

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A. A. Krylov

Budker Institute of Nuclear Physics

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К. А. Савко

Voronezh State University

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П. С. Козлов

V.S. Sobolev Institute of Geology and Mineralogy

S. V. Zinoviev

V.S. Sobolev Institute of Geology and Mineralogy

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Czech Academy of Sciences, Institute of Geology

Siberian Branch of the Russian Academy of Sciences

Russian Academy of Sciences

V.S. Sobolev Institute of Geology and Mineralogy

Zavaritsky Institute of Geology and Geochemistry

Budker Institute of Nuclear Physics

Fiber Optics Research Center

Prokhorov General Physics Institute

Université de Lille

University of Southampton

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The first petrological evidence of subduction at the western margin of the Siberian сraton

Доклады Академии наук (2019)

I I П. С. Козлов К. А. Савко S. V. Zinoviev A. A. Krylov

The discovery of relics of glaucophane schist in high-pressure tectonites of the suture zone of Yenisei Ridge has provided evidence for a Cordillera-type convergent boundary controlled by subduction of the oceanic crust beneath the continental margin on the western side of the Siberian Craton. According to the microtextural patterns of rocks and the results of geothermobarometry, two stages of metamorphism were distinguished. The formation of high-pressure tectonites indicates the early stage in the evolution of the Paleoasian Ocean and the final stage in the Neoproterozoic history of the Yenisei Ridge including completion of the accretion–subduction processes on the western margin of the Siberian Craton.

Tectonite

10.31857/s0869-56524842209-214

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