STRUCTURAL EVOLUTION OF THE CHEKA PLUTON (SOUTHERN URALS): PETROMAGNETIC STUDIES AND FRACTURE ANALYSIS

The Cheka pluton, located in the Magnitogorsk megazone of the Southern Urals and composed of the alkaline granitoids, is meridionally elongated (1–2)×6.5 km. The fracture and anisotropy of magnetic susceptibility analysis was made on the Cheka pluton for the first time. The study materials comprise...

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Bibliographic Details
Main Authors:	P. A. Shestakov, A. Yu. Kazansky, A. V. Tevelev, N. V. Pravikova, E. V. Koptev, E. A. Volodina, A. A. Borisenko, I. A. Kosheleva
Format:	Article
Language:	English
Published:	Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2024-12-01
Series:	Геодинамика и тектонофизика
Subjects:	southern urals granitoids fracture analysis petromagnetic studies strike-slip-fault magmatic duplex structural model magnitogorsk megazone strike-slip fault-related extension
Online Access:	https://www.gt-crust.ru/jour/article/view/1952
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STRUCTURAL EVOLUTION OF THE CHEKA PLUTON (SOUTHERN URALS): PETROMAGNETIC STUDIES AND FRACTURE ANALYSIS

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