Melting conditions of granitoid xenoliths in contact with alkaline mafic magma (Gusinoozerskaya Dyke, Western Transbaikalia) › Research Explorer

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Melting conditions of granitoid xenoliths in contact with alkaline mafic magma (Gusinoozerskaya Dyke, Western Transbaikalia): To the problem of the origin of ultrapotassic acid melts

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

DOI

https://doi.org/10.5800/GT-2017-8-2-0245
Final published version

V. B. Khubanov
T. T. Vrublevskaya
A. A. Tsygankov
A. G. Vladimirov
M. D. Buyantuev
E. N. Sokolova
V. F. Posokhov
E. A. Khromova

Original language	English
Pages (from-to)	347-368
Number of pages	22
Journal	Geodynamics and Tectonophysics
Volume	8
Issue number	2
DOIs	https://doi.org/10.5800/GT-2017-8-2-0245
Publication status	Published - 1 Jan 2017

OECD FOS+WOS

Research areas

Alkaline mafic magma, Calc-alkaline lamprophyre, Contact melting, Granitoid xenoliths, Gusinoozerskaya dyke, Petrogenetic and tectonic conditions, Transbaikalia, Ultrapotassic acidic melt

ID: 9975759