Abstract
The western Baikal region (Ol’khon region, Nutgei zone, Kharikta area) is characterized by the development of packets of thrust-type folds and synkinematic granites corresponding to the stage of thrust deformations (overthrust-type granites). Two stages in the formation of thrust-type folds separated by episodes of granite emplacement are definable. The data obtained make it possible to estimate both the time of transition from thrust to strike-slip deformations and the duration of accretionary‒collisional events that resulted in regional strike-slip deformations, which terminated in the western Baikal region 460‒455 Ma ago.
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Original Russian Text © E.I. Mikheev, A.G. Vladimirov, V.S. Fedorovsky, T.B. Bayanova, A.M. Mazukabzov, A.V. Travin, N.I. Volkova, S.V. Khromykh, V.V. Khlestov, P.A. Tishin, 2017, published in Doklady Akademii Nauk, 2017, Vol. 472, No. 5, pp. 551–557.
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Mikheev, E.I., Vladimirov, A.G., Fedorovsky, V.S. et al. Age of overthrust-type granites in the accretionary‒collisional system of the early Caledonides (western Baikal region). Dokl. Earth Sc. 472, 152–158 (2017). https://doi.org/10.1134/S1028334X17020167
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DOI: https://doi.org/10.1134/S1028334X17020167