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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.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

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

APA

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

Vancouver

Mikheev EI, Vladimirov AG, Fedorovsky VS, Bayanova TB, Mazukabzov AM, Travin AV и др. Age of overthrust-type granites in the accretionary‒collisional system of the early Caledonides (western Baikal region). Doklady Earth Sciences. 2017 февр. 1;472(2):152-158. doi: 10.1134/S1028334X17020167

Author

Mikheev, E. I. ; Vladimirov, A. G. ; Fedorovsky, V. S. и др. / Age of overthrust-type granites in the accretionary‒collisional system of the early Caledonides (western Baikal region). в: Doklady Earth Sciences. 2017 ; Том 472, № 2. стр. 152-158.

BibTeX

@article{07d7874a6bae4daab88baa5ab993aac5,
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.}",
year = "2017",
month = feb,
day = "1",
doi = "10.1134/S1028334X17020167",
language = "English",
volume = "472",
pages = "152--158",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Age of overthrust-type granites in the accretionary‒collisional system of the early Caledonides (western Baikal region)

AU - Mikheev, E. I.

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.

PY - 2017/2/1

Y1 - 2017/2/1

N2 - 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.

AB - 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.

UR - http://www.scopus.com/inward/record.url?scp=85018496955&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17020167

DO - 10.1134/S1028334X17020167

M3 - Article

AN - SCOPUS:85018496955

VL - 472

SP - 152

EP - 158

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 10347715