To a morphogenetic type of Yantyshevsko-Juluksky fault (southern Urals)
Abstract
The structure of the Yantyshevsko-Juluksky fault which is dividing maksut and suvanak metamorphic complexes forming Uraltau zone (Southern Urals) is examined. This fault is proved not to be an east-vergent back thrust, according to the results of investigation of mezostructural paragenezises of folds developed in the zone of dynamic influence of the southern part of the Jantushevsko- Juluksky fault. A new model proposing that this fault is a deformed thrust in which zone rocks of the suvanak complex were thrown from east to the west over metamorphic rocks of the maksut complex.
About the Author
B. G. Golionko
Geological Institute of Russian Academy of Science
Russian Federation
Russian Federation
References
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Review
For citations:
Golionko B.G. To a morphogenetic type of Yantyshevsko-Juluksky fault (southern Urals). Proceedings of higher educational establishments. Geology and Exploration. 2016;(3):8-12. (In Russ.)
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