Collisional metamorphism as a result of thrusting in the Transangara region of the Yenisei Ridge

The Yenisei Ridge is one of the most interesting regions in the southwestern folded framework of the Siberian Craton with respect to geodynamics. The regional structure of the Transangara sector of the Yenisei Ridge is traditionally displayed as a NW-trending system of tectonic sheets divided by fau...

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Veröffentlicht in:	Doklady earth sciences 2006-11, Vol.411 (1), p.1313-1317
Hauptverfasser:	Likhanov, I. I., Kozlov, P. S., Popov, N. V., Reverdatto, V. V., Vershinin, A. E.
Format:	Artikel
Sprache:	eng
Schlagworte:	Metamorphic rocks Metamorphism
Online-Zugang:	Volltext
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