High-Pressure Tectonites of Yenisei Ridge as a Result of Ductile Shear Fault Deformations in the Suture Zone › Research Explorer

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High-Pressure Tectonites of Yenisei Ridge as a Result of Ductile Shear Fault Deformations in the Suture Zone

Research output: Contribution to journal › Article › peer-review

Section of General and Regional Geology

DOI

https://doi.org/10.1134/S1028334X18120061
Final published version

I. I. Likhanov
P. S. Kozlov
K. S. Ivanov
S. V. Zinoviev

Original language	English
Pages (from-to)	1495-1498
Number of pages	4
Journal	Doklady Earth Sciences
Volume	483
Issue number	2
DOIs	https://doi.org/10.1134/S1028334X18120061
Publication status	Published - 1 Dec 2018

Research areas

GARNET, EVOLUTION, GEOBAROMETRY, EXHUMATION, ASSEMBLAGE, EVENTS, AGE

OECD FOS+WOS

ID: 18632039