MECHANISMS OF MANTLE‐CRUST INTERACTION AT DEEP LEVELS OF COLLISION OROGENS (CASE OF THE OLKHON REGION, WEST PRIBAIKALIE)

MECHANISMS OF MANTLE‐CRUST INTERACTION AT DEEP LEVELS OF COLLISION OROGENS (CASE OF THE OLKHON REGION, WEST PRIBAIKALIE)

In the Chernorud granulite zone in the Olkhon region of West Pribaikalie, we studied gabbro‐pyroxenites composing tectonic plates (Chernorud, Tonta) and synmetamorphic intrusive bodies (Ulan‐Khargana), as well as nu‐ merous disintegrated boudins and inclusions embedded in the metamorphic matrix. Bas...

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Bibliographic Details
Main Authors: A. G. Vladimirov, A. S. Mekhonoshin, S. V. Khromykh, E. I. Mikheev, A. V. Travin, N. I. Volkova, T. B. Kolotilina, Yu. A. Davydenko, E. V. Borodina, V. V. Khlestov
Format: Article
Language:English
Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2017-06-01
Series:Геодинамика и тектонофизика
Subjects:
granulite metamorphism
synmetamorphic gabbro‐pyroxenite
hypersthene plagiogranite
stress granite
mantle‐crust interaction
metamorphic magma‐mingling
chernorud granulite zone
olknon region
west pribaikalie
Online Access:https://www.gt-crust.ru/jour/article/view/361

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https://www.gt-crust.ru/jour/article/view/361

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