Age of overthrust-type granites in the accretionary‒collisional system of the early Caledonides (western Baikal region)

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

doi:10.1134/S1028334X17020167

Age of overthrust-type granites in the accretionary‒collisional system of the early Caledonides (western Baikal region)

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

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

1 Цитирования (Scopus)

Аннотация

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.

Язык оригинала	английский
Страницы (с-по)	152-158
Число страниц	7
Журнал	Doklady Earth Sciences
Том	472
Номер выпуска	2
DOI	https://doi.org/10.1134/S1028334X17020167
Состояние	Опубликовано - 1 февр. 2017

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10.1134/S1028334X17020167

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Mikheev, E. I., Vladimirov, A. G., Fedorovsky, V. S., Bayanova, T. B., Mazukabzov, A. M., Travin, A. V., Volkova, N. I., Khromykh, S. V., Khlestov, V. V., & Tishin, P. A. (2017). Age of overthrust-type granites in the accretionary‒collisional system of the early Caledonides (western Baikal region). Doklady Earth Sciences, 472(2), 152-158. https://doi.org/10.1134/S1028334X17020167

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title = "Age of overthrust-type granites in the accretionary‒collisional system of the early Caledonides (western Baikal region)",

abstract = "The western Baikal region (Ol{\textquoteright}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.",

author = "Mikheev, {E. I.} and Vladimirov, {A. G.} and Fedorovsky, {V. S.} and Bayanova, {T. B.} and Mazukabzov, {A. M.} and Travin, {A. V.} and Volkova, {N. I.} and Khromykh, {S. V.} and Khlestov, {V. V.} and Tishin, {P. A.}",

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Mikheev, EI, Vladimirov, AG, Fedorovsky, VS, Bayanova, TB, Mazukabzov, AM, Travin, AV, Volkova, NI, Khromykh, SV, Khlestov, VV & Tishin, PA 2017, 'Age of overthrust-type granites in the accretionary‒collisional system of the early Caledonides (western Baikal region)', Doklady Earth Sciences, том. 472, № 2, стр. 152-158. https://doi.org/10.1134/S1028334X17020167

Age of overthrust-type granites in the accretionary‒collisional system of the early Caledonides (western Baikal region). / Mikheev, E. I.; Vladimirov, A. G.; Fedorovsky, V. S. и др.

В: Doklady Earth Sciences, Том 472, № 2, 01.02.2017, стр. 152-158.

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

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AU - Vladimirov, A. G.

AU - Fedorovsky, V. S.

AU - Bayanova, T. B.

AU - Mazukabzov, A. M.

AU - Travin, A. V.

AU - Volkova, N. I.

AU - Khromykh, S. V.

AU - Khlestov, V. V.

AU - Tishin, P. A.

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