Mechanisms of mantle-crust interaction at deep levels of collision orogens (case of the Olkhon region, West Pribaikalie)

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

Original language	English
Pages (from-to)	223-268
Number of pages	46
Journal	Geodynamics and Tectonophysics
Volume	8
Issue number	2
DOIs	https://doi.org/10.5800/GT-2017-8-2-0240
Publication status	Published - 1 Jan 2017

Chernorud granulite zone, Granulite metamorphism, Hypersthene plagiogranite, Mantle-crust interaction, Metamorphic magma-mingling, Olknon region, Stress granite, Synmetamorphic gabbro-pyroxenite, West Pribaikalie, IGNEOUS ROCKS, SYSTEM, EARLY CALEDONIDES, GEODYNAMICS, synmetamorphic gabbro-pyroxenite, TECTONIC POSITION, metamorphic magma-mingling, CONVERGENT BOUNDARIES, mantle-crust interaction, LAKE BAIKAL, GRANITOID MAGMATISM, granulite metamorphism, MODEL, hypersthene plagiogranite, OPTIMIZED STANDARD STATE, stress granite

ID: 9975698